Station_ID	Visit_date	Lat_NAD83	Long_NAD83	Coord_meth	Collector	Lead_geo	MS_min	MS_avg	MS_max	cps_min	cps_avg	cps_max	K_pct_gsp	Th_ppm_gsp	U_ppm_gsp	Stat_note	Lith1_occ	Rock_cls1	Lith1	L1_M1	L1_M1_pct	L1_M2	L1_M2_pct	L1_M3	L1_M3_pct	L1_colour	L1_rck_fab	L1_texture	L1_xtal_sz	Lith1_note	Lith2_occ	Rock_cls2	Lith2	L2_M1	L2_M1_pct	L2_M2	L2_M2_pct	L2_M3	L2_M3_pct	L2_colour	L2_rck_fab	L2_texture	L2_xtal_sz	Lith2_note	Struc1_typ	S1_azimuth	S1_dip	S1_intnsty	S1_note	Struc2_typ	S2_azimuth	S2_dip	S2_intnsty	S2_note	Struc3_typ	S3_azimuth	S3_dip	S3_intnsty	S3_note	Smp1_ID	Smp1_anlys	Smp1_note	Smp2_ID	Smp2_anlys	Smp2_note	Smp3_ID	Smp3_anlys	Smp3_note	Smp4_ID	Smp4_anyls	Smp4_note	Publisher
AL-23-1104	04-07-2023 14:34:20.373	59.853729	-110.103563	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.19	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.19.	main lithology	granitoid	granodiorite	biotite	5-10%	hornblende	1-5%	-9999	-9999	white	foliated	porphyritic	phaneritic coarse (5-10mm)	No notes captured.	dike	granitoid	pegmatite dike	feldspar	>50%	quartz	20-50%	-9999	-9999	buff	massive	-9999	pegmatitic	dike of pegmatite that cross cuts foliation.	FOL1 - Foliation gen1	205	68	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1104-1	whole-rock lithogeochemistry; thin section	Contact between granodiorite and pegmatite.	AL-23-1104-2	whole-rock lithogeochemistry	Sample of granodiorite.	AL-23-1104-3	whole-rock lithogeochemistry	Granodiorite, but from a different part of the outcrop.	AL-23-1104-4	whole-rock lithogeochemistry	Pegmatite dike, small sample.	Alberta Geological Survey
AL-23-1105	04-07-2023 16:49:17.603	59.843914	-110.112492	Internal GPS	Calla Knudson	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	quartz	20-50%	plagioclase	20-50%	alkali-feldspar	20-50%	grayish white	foliated	equigranular	phaneritic coarse (5-10mm)	Leucogranite. Very homogeneous. Thin quartz stringers. No visible mafic minerals. Fine-grained biotite (1-5%). Alkali spar slightly more abundant than plagioclase.	sheet	schist	intermediate schist	biotite	20-50%	quartz	20-50%	-9999	-9999	-9999	schistose	equigranular	phaneritic medium (1-5mm)	Leucogranitic injection.	FOL - Foliation	210	71	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1105-1	whole-rock lithogeochemistry	Leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1106	05-07-2023 09:41:39.425	59.839621	-110.131654	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.25	-9999	-9999	-9999	500	-9999	-9999	-9999	Mylonite is a granite composition with a small amount of dismembered amphibolite and pegmatite.  Island outcrop initial plotting is wrong location but edited. Measurements - MS 0.25; Scint up to 500 cps.	main lithology	mylonite	mesomylonite	chlorite	1-5%	-9999	-9999	-9999	-9999	white to pinkish	foliated	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	215	62	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1106-1	whole-rock lithogeochemistry	Example of mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1107	05-07-2023 10:39:37.699	59.830220	-110.139193	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Very large outcrop area along the north part of the island. Very consistent.	main lithology	mylonite	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	equigranular	phaneritic medium (1-5mm)	Uranium city style pink granitoid. One mafic flattened xenoliths.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	345	77	Foliation strong	-9999	VN - Vein	110	70	-9999	Quartz.	FOL2 - Foliation gen2	10	69	Foliation strong	Foliation overprinting S1.	AL-23-1107-1	whole-rock lithogeochemistry	Granitoid mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1108	05-07-2023 11:45:32.717	59.836942	-110.125037	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.15.	main lithology	gneiss	granite	biotite	10-20%	-9999	-9999	-9999	-9999	buff to white	gneissic	-9999	phaneritic medium (1-5mm)	Ghosty gneissosity with rare folding and pods and thin sheets of pegmatite. There is one amphibolite xenolith. Rock looks granular.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	335	36	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1109	05-07-2023 12:20:10.272	59.834261	-110.119263	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	4	-9999	-9999	-9999	-9999	-9999	-9999	Heterogenous in places with biotite rich sheets that are smeared out.	main lithology	gneiss	granite	biotite	10-20%	-9999	-9999	-9999	-9999	pink to buff	gneissic	-9999	phaneritic coarse (5-10mm)	MS up to 4. Pegmatitic patches and small amounts of quartz vein. Granular appearance.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	325	78	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1109-1	whole-rock lithogeochemistry	Granitoid gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1110	05-07-2023 13:23:36.783	59.831269	-110.126760	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	paragneiss	biotite	20-50%	sillimanite	<1%	graphite	<1%	grey	gneissic	-9999	-9999	Graphite, crenulated schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	186	74	Foliation strong	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1110-1	whole-rock lithogeochemistry	Paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1111	05-07-2023 14:36:05.862	59.819320	-110.132283	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.17	-9999	-9999	200	320	-9999	-9999	-9999	Looks like a quartzite/psammite.  Lots of folding and disruption of layers. Measurements - average of 200 cps; High of 320cps; MS 0.17.	main lithology	gneiss	paragneiss	biotite	10-20%	garnet	<1%	sillimanite	<1%	white and rusty	gneissic	-9999	-9999	Some biotite rich layers. Look at thin section.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	45	70	Foliation strong	Folding of outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1111-1	whole-rock lithogeochemistry; thin section	Main lithology, psammite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1112	05-07-2023 15:23:21.315	59.821456	-110.123600	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Granular recrystallized.	main lithology	mylonite	granite	biotite	5-10%	-9999	-9999	-9999	-9999	pink to white	foliated	-9999	-9999	Homogeneous, beaded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	STR - Glacial stria	242	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1113	05-07-2023 16:04:00.614	59.857340	-110.100414	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Recessive weathering. Chewed up pegmatite in part. Just boudin and porphyroclasts.	main lithology	gneiss	paragneiss	biotite	5-10%	sillimanite	1-5%	-9999	-9999	grey, white, and rusty	gneissic	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	200	62	Foliation strong	Folded at outcrop. Goes to opposite dip in places.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1113-1	whole-rock lithogeochemistry; thin section	Paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1114	06-07-2023 10:07:38.478	59.816909	-110.281763	Internal GPS	Russell Hartlaub	Russell Hartlaub	7	-9999	20	-9999	-9999	260	-9999	-9999	-9999	Measurements - MS 7 to 20; Scint max is 260 cps.	main lithology	gneiss	granite	biotite	10-20%	chlorite	1-5%	magnetite	<1%	pink with green zones	gneissic	-9999	phaneritic coarse (5-10mm)	Rock contains a strongly foliated gneiss component with cm to 1/2 m pegmatitic and granitic layers.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	166	80	Foliation strong	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1114-1	whole-rock lithogeochemistry	Main gneissic granitoid.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1115	06-07-2023 11:03:30.270	59.816631	-110.277759	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	134	-9999	249	-9999	-9999	-9999	Measurements - Scint avg 134 cps to 249 cps.	main lithology	gneiss	granite	biotite	10-20%	magnetite	<1%	-9999	-9999	pink and locally hematized	gneissic	-9999	phaneritic coarse (5-10mm)	Some bioite rich zones. There is a yellow oxidizing mineral in trace amounts that was also in the last outcrop. Thin section to determine.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	15	74	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1115-1	whole-rock lithogeochemistry; thin section	What is yellow weathering trace mineral. Geochem anomalies of Godfrey at this location.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1116	06-07-2023 11:50:38.944	59.818146	-110.288760	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	480	-9999	-9999	-9999	Scint high of 480 cps on a white altered patch of the gneiss.	main lithology	gneiss	granite	biotite	10-20%	magnetite	<1%	-9999	-9999	pink to grey	gneissic	-9999	-9999	More heterogeneous than previous outcrop. Pegmatitic patches include some that are sub-parallel to foliation.	xenolith	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	200	64	Foliation strong	-9999	LINF - Lineation fold	175	40	-9999	-9999	AXF - Axial fold plane	358	73	-9999	-9999	AL-23-1116-1	whole-rock lithogeochemistry	High cps layer in gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1117	06-07-2023 13:39:33.804	59.825891	-110.298889	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	2000	-9999	-9999	-9999	Pegmatite dike with scint above 2000 cps. Coarse to very coarse grained dike with biotite. Quartz rich. Non foliated.	main lithology	gneiss	paragneiss	biotite	10-20%	garnet	<1%	cordierite	<1%	gray and rusty	schistose	-9999	-9999	Cordierite? Pegmatite dike cuts at roughly 190/65. Not foliated.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	10	68	-9999	-9999	VN - Vein	200	40	-9999	Quartz vein.	-9999	-9999	-9999	-9999	-9999	AL-23-1117-1	whole-rock lithogeochemistry; thin section	Pegmatite dike containing biotite that cross cuts foliation and has high CPS on scintillometer.	AL-23-1117-2	whole-rock lithogeochemistry; thin section	Paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1118	06-07-2023 14:44:55.372	59.831179	-110.293179	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.2	-9999	-9999	-9999	400	-9999	-9999	-9999	Strongly hematized. Measurements - Scint up to 400 cps; MS 0.2.	main lithology	mylonite	granite	chlorite	10-20%	epidote	1-5%	-9999	-9999	red hematite	foliated	-9999	phaneritic medium (1-5mm)	Ribboned quartz in mylonite. Uranium City style.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	red	massive	-9999	pegmatitic	Pegmatitic layers in the mylonite.	FOL1 - Foliation gen1	35	70	Foliation intense	1 mm ribbons.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1118-1	whole-rock lithogeochemistry	Mylonitic granite with chlorite and epidote. Hematitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1119	06-07-2023 15:30:12.492	59.833493	-110.301848	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	300	-9999	500	-9999	-9999	-9999	Measurements - Scint around 300 cps - 500 cps.	main lithology	gneiss	paragneiss	garnet	<1%	cordierite	<1%	biotite	5-10%	grey to buff	foliated	-9999	phaneritic medium (1-5mm)	Compositional layering bands of biotite rich material.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	buff	-9999	-9999	-9999	Scint does not jump up at this pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1119-1	whole-rock lithogeochemistry	Pegmatite that injects the gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1120	06-07-2023 16:12:44.456	59.834160	-110.298035	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	1.8	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strongly hematized. Measurements - MS 1.8; Scint is low cps.	main lithology	mylonite	granite	chlorite	5-10%	quartz	10-20%	-9999	-9999	pink and hematite red	foliated	-9999	phaneritic medium (1-5mm)	Recrystalized mylonite. Some xenoliths/ schlieren of dark biotitic nature.	sheet	granitoid	pegmatite dike	-9999	-9999	-9999	-9999	-9999	-9999	red	-9999	-9999	pegmatitic	Hematized pegmatite layer.	FOL1 - Foliation gen1	25	68	Foliation intense	Folded across outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1120-1	whole-rock lithogeochemistry	Sheared granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1121	06-07-2023 16:53:12.479	59.820443	-110.297337	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	1170	-9999	-9999	-9999	Island. Strongly hematized.  MS 0.15, scint up to 555 cps in granite but one pegmatitic area is around 1170 cps.	main lithology	mylonite	granite	chlorite	1-5%	-9999	-9999	-9999	-9999	hematitic red	-9999	-9999	-9999	Leucocratic portion of the outcrop looks to be late (sample 1).	sheet	schist	intermediate schist	biotite	20-50%	chlorite	5-10%	-9999	-9999	green grey	-9999	-9999	-9999	Mafic appearing xenoliths in the leucocratic granite.	FOL1 - Foliation gen1	280	71	Foliation strong	Folding in outcrop. This foliation is on east side of island.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1121-1	whole-rock lithogeochemistry	Leucocratic component of granite.	AL-23-1121-2	whole-rock lithogeochemistry; thin section	Chloritic component (layer, xenoliths).	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1122	06-07-2023 17:33:39.565	59.818308	-110.295783	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Highly fractured. Locally Hematitic. One dark xenolith. Recrystallized.	main lithology	mylonite	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink and hematite	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	345	75	Foliation strong	Folded so foliation wraps around.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1123	07-07-2023 10:44:19.882	59.821740	-110.209107	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.16	10	-9999	-9999	-9999	-9999	-9999	-9999	Beautiful injection of leucogranite into amphibolite and gneiss.  THERE ARE THREE UNITS HERE! ORTHOGNEISS (oldest), LEUCOGRANITE, and AMPHIBOLITE/MAFIC SCHIST (younger than gneiss, weakly foliated, but age relationship with leucogranite is not clear). Measurements - Scint is low. MS 0.16 (but locally up to 10).  	main lithology	gneiss	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	gneissic	-9999	-9999	Oldest unit.	dike	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Disrupted and injected(?) by leucogranite.  Leucogranite likely same age as pegmatites in the outcrop.	FOL1 - Foliation gen1	232	52	Foliation strong	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1123-1	whole-rock lithogeochemistry; thin section	Amphibolite/fine grained mafic rock.	AL-23-1123-2	whole-rock lithogeochemistry	Leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1124	07-07-2023 11:18:24.829	59.822004	-110.208768	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large expanse of fine grained mafic that intrudes the gneiss. Rotated block of gneiss.	main lithology	mafic rocks	mafic schist	hornblende	20-50%	-9999	-9999	-9999	-9999	dark grey	foliated	equigranular	phaneritic fine (0.5-1mm)	Contains rotated gneiss block.	minor lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	331	69	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1124-1	whole-rock lithogeochemistry	Mafic schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1125	07-07-2023 11:42:14.749	59.822893	-110.207860	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge pink outcrop.	main lithology	granitoid	granite	biotite	5-10%	magnetite	<1%	-9999	-9999	pink	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	205	65	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1125-1	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1126	07-07-2023 12:05:40.343	59.824768	-110.205857	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	500	-9999	-9999	-9999	Measurements - Scint 500 cps.	main lithology	granitoid	granite	magnetite	<1%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	All granite from last outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	200	56	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1127	07-07-2023 12:21:15.548	59.825752	-110.204766	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.08	-9999	-9999	-9999	1725	-9999	-9999	-9999	Outcrop is hematized.  Measurements - cps locally up to 1725.  MS 0.08.	main lithology	granitoid	granite	biotite	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	170	76	Foliation strong	Gneiss is locally and folded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1127-1	whole-rock lithogeochemistry	Pink granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1128	07-07-2023 13:13:25.448	59.827583	-110.203388	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	172	62	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1129	07-07-2023 13:45:29.872	59.828412	-110.203742	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	1700	-9999	-9999	-9999	Pegmatite, scint up to 1700 cps.	main lithology	gneiss	orthogneiss	biotite	10-20%	magnetite	<1%	-9999	-9999	banded pink and grey	gneissic	-9999	phaneritic coarse (5-10mm)	Mm to cm scale bands. Looks like the oldest component I have seen today. Cut by pegmatite.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	massive	-9999	pegmatitic	No notes captured.	FOL1 - Foliation gen1	205	79	Foliation strong	Gneiss if banding.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1129-1	whole-rock lithogeochemistry	Poor sample of the cross cutting pegmatite that has cps up to 1700. Need a saw.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1130	07-07-2023 14:33:19.083	59.829325	-110.204261	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	600	4500	-9999	-9999	-9999	Main rock is the recrystalized granite mylonite. Noted mineral occurrence. Huge outcrop but lots of lichen cover.  Up to 4500 cps with a background of >600 cps. One band is dark and looks dioritic with high cps, sampled.	main lithology	mylonite	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	No notes captured.	minor lithology	gneiss	mafic gneiss	feldspar	20-50%	biotite	20-50%	-9999	-9999	black and white	foliated	equigranular	phaneritic medium (1-5mm)	Band with high cps. Plag phenocrysts?	FOL1 - Foliation gen1	192	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1130-1	whole-rock lithogeochemistry; thin section	Mafic, high cps.	AL-23-1130-2	whole-rock lithogeochemistry; thin section	This has high cps, but from a different layer 15m along strike.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1131	07-07-2023 15:14:41.535	59.828431	-110.206154	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	biotite	10-20%	magnetite	<1%	-9999	-9999	pink banded with black	gneissic	-9999	phaneritic coarse (5-10mm)	Cut by 10% pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	204	80	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1131-1	whole-rock lithogeochemistry	Pegmatitic zone within gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1132	07-07-2023 15:39:28.562	59.826780	-110.207595	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quick station, gneissic granite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1133	07-07-2023 15:52:12.984	59.825784	-110.206285	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	dike	granitoid	granite	alkali-feldspar	20-50%	quartz	20-50%	-9999	-9999	pink	-9999	-9999	pegmatitic	Pegmatite cutting gneiss. Good spot for sample. Unidentified black mineral. 50 cm wide. At edge of outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1133-1	whole-rock lithogeochemistry	Cross cutting pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1134	09-07-2023 09:03:41.305	59.805644	-110.225799	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	21	-9999	-9999	200	850	-9999	-9999	-9999	Measurements - Scint up to 850 cps at shore, only 200 cps up the hill; MS 21.	main lithology	gneiss	orthogneiss	magnetite	<1%	biotite	10-20%	-9999	-9999	buff	gneissic	equigranular	phaneritic coarse (5-10mm)	This is the older? More biotitic granodiorite component.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Locally pegmatitic.	FOL1 - Foliation gen1	250	82	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1134-1	whole-rock lithogeochemistry	Pegmatitic layer (809 cps) in the gneiss.	AL-23-1134-2	whole-rock lithogeochemistry	The granodiorite component.  200 cps.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1135	09-07-2023 10:25:51.661	59.812110	-110.233828	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	11.5	-9999	-9999	260	380	-9999	-9999	-9999	Cross cutting pegmatite, 260 cps, and 380 cps measurements.  Ms 11.5.	main lithology	gneiss	orthogneiss	biotite	10-20%	magnetite	<1%	-9999	-9999	buff	gneissic	-9999	-9999	Banded gneiss.	dike	granitoid	granite	alkali-feldspar	20-50%	-9999	-9999	-9999	-9999	pink	massive	-9999	pegmatitic	Cross cutting pegmatite.	FOL1 - Foliation gen1	66	44	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1135-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1136	09-07-2023 10:59:13.533	59.805642	-110.222446	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.2	-9999	0.4	-9999	-9999	200	-9999	-9999	-9999	Measurements - Scint avg 200 cps; MS 0.2 to 0.4.	main lithology	gneiss	granodiorite	biotite	10-20%	epidote	1-5%	-9999	-9999	buff	gneissic	-9999	-9999	Main banded gneiss cut by the granite.	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Ranges to pegmatitic. Clearly cutting gneissosity.	FOL1 - Foliation gen1	265	50	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1136-1	whole-rock lithogeochemistry; thin section	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1137	09-07-2023 11:37:34.289	59.807840	-110.205594	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.4	-9999	15	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 15 (in gneiss); MS 0.4 (in granite).	main lithology	granitoid	granite	biotite	5-10%	chlorite	1-5%	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Locally pegmatitic.	minor lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	200	73	Foliation moderate	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1137-1	whole-rock lithogeochemistry	Granitic component.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1138	09-07-2023 12:43:09.035	59.807358	-110.198774	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	4.5	-9999	-9999	300	1000	-9999	-9999	-9999	Measurements - MS 4.5; Scint avg 300 cps (except at a cross-cutting pegmatite where more than 1000 cps). Flagged to come back and collect with rock saw.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	218	51	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1138-1	whole-rock lithogeochemistry	Gneissic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1139	09-07-2023 13:12:13.059	59.803121	-110.194685	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	25.5	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 25.5.	main lithology	granitoid	granite	magnetite	<1%	-9999	-9999	-9999	-9999	pink	gneissic	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1140	09-07-2023 13:18:27.519	59.803812	-110.193242	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pure outcrop from boat.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Locally pegmatitic granite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Injected by granite.	FOL1 - Foliation gen1	225	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1140-1	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1141	09-07-2023 13:29:38.519	59.804153	-110.192834	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Crazy amount of folding here.	main lithology	gneiss	granite	biotite	10-20%	-9999	-9999	-9999	-9999	pink hematite	gneissic	-9999	-9999	Looks sheared and then folded. Axial planar quartz veining.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	220	52	-9999	-9999	FOL2 - Foliation gen2	290	75	Foliation moderate	Quartz veining aligned to S2.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1142	09-07-2023 13:48:35.890	59.805692	-110.191386	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	430	-9999	-9999	-9999	Same layered granitic gneiss here. All the way from the boat.	main lithology	gneiss	granite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	-9999	-9999	phaneritic coarse (5-10mm)	Up to 430 cps, sheared like previous 2 outcrop with lots of folding.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1142-1	whole-rock lithogeochemistry	Biotite rich. There are no mafic xenoliths or layers.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1143	09-07-2023 14:15:25.527	59.805943	-110.192428	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	1500	-9999	-9999	-9999	Measurements - Scint max 1500 cps on this outcrop, but impossible to get a good sample of the high zone.	main lithology	gneiss	granite	chlorite	1-5%	biotite	10-20%	-9999	-9999	pink and green darker hematite	foliated	-9999	-9999	Lichen covered.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	225	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1143-1	whole-rock lithogeochemistry	Not from high cps section.	AL-23-1143-2	whole-rock lithogeochemistry	Same material as sample 1, 10 m away.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1144	09-07-2023 14:55:36.824	59.795537	-110.194890	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.4	-9999	-9999	-9999	400	-9999	-9999	-9999	Strongly banded gneiss with lots of folding.  On south side of the bay.  Granite injection makes up about 50%.	main lithology	gneiss	orthogneiss	magnetite	<1%	biotite	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	epidote	<1%	-9999	-9999	-9999	-9999	bright pink and hematized	-9999	equigranular	phaneritic coarse (5-10mm)	Measurements - MS 0.4; Scint max 400 cps.	FOL1 - Foliation gen1	210	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1144-1	whole-rock lithogeochemistry; thin section	Orthogneiss, possibly representative of the oldest basement gneiss, large sample collected suitable for geochronology.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1145	09-07-2023 15:38:58.388	59.812154	-110.232993	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	15	-9999	-9999	-9999	1500	-9999	-9999	-9999	Pegmatite dike shows 1500 cps. Easy to collect.	dike	granitoid	granite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	massive	-9999	pegmatitic	Pegmatite dike up to 1500 cps.	main lithology	granitoid	granite	magnetite	<1%	biotite	10-20%	-9999	-9999	-9999	foliated	-9999	phaneritic coarse (5-10mm)	This coarse grained foliated granite is cut by the pegmatite. Measurements - MS 15.	FOL1 - Foliation gen1	215	78	Foliation moderate	-9999	LINM - Lineation mineral	220	35	Foliation moderate	The granitoid is lineated. There is some banded gneiss to the east.	-9999	-9999	-9999	-9999	-9999	AL-23-1145-1	whole-rock lithogeochemistry; thin section	Three large samples. Cuts a foliated coarse grained granitoid.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1146	10-07-2023 09:24:30.157	59.816267	-110.296781	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.17	-9999	-9999	-9999	1500	-9999	-9999	-9999	Measurements - Scint max 1500 cps on peg dike; MS 0.17 (schist).	main lithology	schist	intermediate schist	biotite	20-50%	quartz	20-50%	-9999	-9999	grey	schistose	-9999	phaneritic medium (1-5mm)	A schistose folded rock with numerous felsic and thin granitic bands that has been folded. It is cut by the granite pegmatite.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pale pink	-9999	-9999	pegmatitic	Cuts the foliation.	FOL1 - Foliation gen1	195	60	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1146-1	whole-rock lithogeochemistry	Homogenous part of schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1147	10-07-2023 09:50:47.503	59.815781	-110.296667	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.3	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.3.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink to grey	schistose	-9999	phaneritic medium (1-5mm)	Disrupted pegmatite in a chlorite bearing fine grained layered fine grained mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	35	80	Foliation intense	Shear layers foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1148	10-07-2023 10:01:34.157	59.815397	-110.296320	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous but with amphibolite.	main lithology	mylonite	mesomylonite	chlorite	1-5%	-9999	-9999	-9999	-9999	pink banded	gneissic	-9999	-9999	Mixed mylonite. Some bands look like quartzite. Seems partially sedimentary here.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	LINF - Lineation fold	190	34	-9999	Lots of close folds.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1149	10-07-2023 10:33:03.787	59.814828	-110.297717	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	16	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous outcrop. Measurements - MS 16 (in mylonite).	main lithology	mylonite	mesomylonite	chlorite	<1%	magnetite	<1%	-9999	-9999	pink and grey cm scale layering	gneissic	-9999	phaneritic medium (1-5mm)	No notes captured.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	No notes captured.	FOL1 - Foliation gen1	18	79	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1149-1	whole-rock lithogeochemistry	Pegmatite that cross cuts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1150	10-07-2023 11:28:41.356	59.814783	-110.298509	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	500	-9999	1000	-9999	-9999	-9999	High cps (500 to 1000 in mixed mylonite gneiss) with pegmatites and a thick 5 m wide amphibolite. Amphibolite lines up along strike with Godfrey map.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	mixed pink and grey	-9999	-9999	phaneritic medium (1-5mm)	No notes captured.	minor lithology	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	green	-9999	-9999	-9999	Contains trace sulfides.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1150-1	whole-rock lithogeochemistry	Biotite rich amphibolite layer.	AL-23-1150-2	whole-rock lithogeochemistry	Chloritic granitoid gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1151	10-07-2023 11:59:05.523	59.813457	-110.300995	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.02	-9999	-9999	-9999	1000	-9999	-9999	-9999	New unit here. White granite. Measurements - MS 0.02; Scint locally up to 1000 cps, but mostly low.	main lithology	granitoid	granite	biotite	5-10%	-9999	-9999	-9999	-9999	white	foliated	-9999	phaneritic coarse (5-10mm)	No hematite here. Outside the shear zone.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	195	78	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1151-1	whole-rock lithogeochemistry	White granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1152	10-07-2023 12:59:44.528	59.813563	-110.302063	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	65000	-9999	-9999	-9999	Maxed scintillometer at 65,000 cps in a gossanous fault zone (known mineral occurrence).  Yellow uranium oxides.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	white to pink	gneissic	-9999	phaneritic coarse (5-10mm)	Ribboned and disrupted granitic rock primarily. Gossanous u-rich zone is parallel to foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	192	64	Foliation intense	Mylonitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1152-1	whole-rock lithogeochemistry	Host rock to the gossanous structure. 1500 cps. Right beside the gossanous zone.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1206	17-07-2023 14:30:08.129	59.903963	-110.067740	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Boundary between the Colin and the diorite runs along the southwest portion of the island.  Colin is on the southwest.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white	massive	equigranular	phaneritic coarse (5-10mm)	No xenoliths of the mafic are visible.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	1	69	-9999	Also the orientation of the boundary.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1207	17-07-2023 15:11:42.822	59.906190	-110.060066	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.05	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.05 in mylonite.	main lithology	mylonite	mesomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	grey to rusty brown	foliated	-9999	-9999	Contact between the mylonite and the massive Colin Lake granite here. Whole west side of island is Mylonite. Porphyroclasts are common.	main lithology	granitoid	granite	muscovite	1-5%	-9999	-9999	-9999	-9999	white	massive	-9999	pegmatitic	Caught up in late stages of shearing. Colin Lake colour.	SH - Shear Ductile	315	49	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1208	17-07-2023 15:47:13.359	59.909365	-110.062805	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge outcrop of homogeneous granite. White. MS 0.00. Colin Lake granite.	main lithology	granitoid	granite	muscovite	1-5%	-9999	-9999	-9999	-9999	white	massive	equigranular	phaneritic coarse (5-10mm)	Looks like the slave granites.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1208-1	whole-rock lithogeochemistry; thin section	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1209	17-07-2023 16:13:04.325	59.902591	-110.057083	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.4	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	First bit of outcrop that we could land on that is clearly our paragneiss unit. 20-40% granitic laters that may be melt.  It’s now folded and dismembered.  MS 0.4 to 1.	main lithology	gneiss	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	rusty and brown	schistose	-9999	-9999	This part of the lake is near devoid of outcrop, so it makes sense that softer sediments are here, but eroded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	358	78	Foliation strong	Schistose.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1209-1	whole-rock lithogeochemistry; thin section	Biotite rich paragneiss/schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2064	04-07-2023 15:16:18.525	59.853367	-110.105726	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Phasing out of granodiorite, into Rutledge River paragneiss, decrease in abundance of feldspar phenocrysts, seeing patches and slivers of sillimanite bearing, biotite rich potential metaseds. Layer parallel pegmatite melt, often associated with biotite selvage, locally extremely biotite rich. Moving east, begin to see cross-cutting granite splits dikes, cutting the pegmatite melts. Increasingly sheared to the east, where sample 3 (aplite-dike) is taken.	main lithology	granitoid	granodiorite	plagioclase	20-50%	biotite	20-50%	-9999	-9999	greyish pink	foliated	porphyritic	phaneritic coarse (5-10mm)	No notes captured.	minor lithology	granitoid	pegmatite sill	alkali-feldspar	>50%	biotite	5-10%	-9999	-9999	-9999	layered	-9999	pegmatitic	White powdery mineral, possibly sericutzed plagioclase.	-9999	10	87	Foliation strong	-9999	AXF - Axial fold plane	340	80	-9999	Associated S2 cleavage oriented in the same direction, in line with the axial plane.	-9999	-9999	-9999	-9999	-9999	AL-23-2064-1	whole-rock lithogeochemistry	Granodiorite.	AL-23-2064-2	whole-rock lithogeochemistry	Pegmatite, layer parallel.	AL-23-2064-3	whole-rock lithogeochemistry	Aplite dike.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1153	10-07-2023 13:36:59.399	59.812176	-110.299875	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large open fold of the mylonite.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	banded white and grey	gneissic	-9999	phaneritic medium (1-5mm)	No notes captured.	main lithology	granitoid	granite	chlorite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	LINF - Lineation fold	80	55	-9999	Large open fold.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1153-1	whole-rock lithogeochemistry	Chloritic granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1154	10-07-2023 14:01:54.096	59.810925	-110.299134	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Sulfides in this outcrop.  Very lichen covered.	main lithology	schist	felsic schist	biotite	10-20%	-9999	-9999	-9999	-9999	grey, locally rusty	schistose	-9999	phaneritic medium (1-5mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	180	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1154-1	whole-rock lithogeochemistry	Felsic schist with sulfides.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1155	10-07-2023 14:28:34.860	59.811602	-110.297460	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.015	-9999	-9999	-9999	700	-9999	-9999	-9999	Measurements - 700 cps. MS 0.015.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white	foliated	-9999	phaneritic coarse (5-10mm)	Nice clean white granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1155-1	whole-rock lithogeochemistry; thin section	White granite. Not gneissic or banded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1156	10-07-2023 14:55:50.397	59.812127	-110.296738	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	1500	-9999	-9999	-9999	No notes captured.	main lithology	schist	felsic schist	-9999	-9999	-9999	-9999	-9999	-9999	white	layered	-9999	-9999	Quartzite and minor schist folded.	dike	granitoid	granodiorite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	pegmatitic	Measurements - Scint 1500 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1156-1	whole-rock lithogeochemistry	Pegmatite cutting a quartz rich rock, quartzite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1157	10-07-2023 15:18:51.666	59.812831	-110.297067	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	black	foliated	equigranular	phaneritic coarse (5-10mm)	Large outcrop of black homogeneous amphibolite injected by pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1157-1	whole-rock lithogeochemistry; thin section	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1158	11-07-2023 09:19:33.664	59.815135	-110.136349	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.5	-9999	30	-9999	-9999	1000	-9999	-9999	-9999	Huge outcrop above beach.  Halo not turning on. Measurements - MS 0.5 to 30 in granite; Scint up to 1000 cps.	main lithology	granitoid	granite	biotite	5-10%	magnetite	<1%	-9999	-9999	pink to white	foliated	porphyritic	phaneritic coarse (5-10mm)	There are two granitoids here. A pink red hematites one on the west White with lots of xenoliths in east. The one on the west may have Relict hornblende and is more mafic. Ground mass of quartz and biotite is medium grained kspar up to 1cm.	main lithology	gneiss	paragneiss	biotite	10-20%	muscovite	1-5%	sillimanite	<1%	mixed grey or buff	layered	-9999	-9999	Good compositional layering.	FOL1 - Foliation gen1	205	80	Foliation moderate	Locally intense foliage on in the granite. But it is mostly weakly foliated.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1158-1	whole-rock lithogeochemistry; thin section	Granite. Red and homogeneous on the west side of outcrop.	AL-23-1158-2	whole-rock lithogeochemistry; thin section	Felsic white granite portion on the east side of outcrop.	AL-23-1158-3	whole-rock lithogeochemistry	Rusty deformed zone of felsic schist.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1159	11-07-2023 10:34:22.373	59.814630	-110.137975	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Sharp boundary between red granite and basement gneiss with pegmatite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Banded.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	2.3 Ga granite, but pegmatitic phase here, magnetic susceptibility 0.2 to 1.5, lower mag then basement gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1160	11-07-2023 10:45:40.326	59.813819	-110.139733	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	2000	-9999	-9999	-9999	Huge clean outcrop. Strongly banded with rotated schlieren in places. Numerous brown biotitic bands. Scint up to 2000. Halo station; Trimble not working despite perfect position.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink with lots of granite	-9999	-9999	-9999	Contains some large bands of amphibolite (sample 3) and is locally high cps (sample 4).	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink to white	foliated	equigranular	phaneritic coarse (5-10mm)	Cut gneissic banding. Sheets of leucocratic granite that cut the gneiss but have been locally folded. Porphyroclastic locally. This area is strongly sheared.	FOL1 - Foliation gen1	210	63	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1160-1	whole-rock lithogeochemistry; thin section	Basement gneiss.	AL-23-1160-2	whole-rock lithogeochemistry	Rusty zone of possible metasediments with 1500 cps.	AL-23-1160-3	whole-rock lithogeochemistry; thin section	Amphibolite.	AL-23-1160-4	whole-rock lithogeochemistry; thin section	Gneiss with 2700 cps.	Alberta Geological Survey
AL-23-1161	11-07-2023 11:59:35.969	59.810713	-110.148424	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	7.5	-9999	400	-9999	500	-9999	-9999	-9999	Huge clean outcrop. Measurements - MS 7.5;  Cps 400-500.	main lithology	gneiss	orthogneiss	magnetite	<1%	biotite	5-10%	-9999	-9999	pink	gneissic	-9999	phaneritic coarse (5-10mm)	Mostly granite with 10-20% mafic zones and schlieren. Possible hornblende converted to biotite. Epidote is locally abundant.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	221	79	Foliation strong	Variable strain.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1161-1	whole-rock lithogeochemistry	Regular banded granitic gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1162	11-07-2023 13:09:35.630	59.810755	-110.150087	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	13	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge outcrop at top of hill. Measurements - MS 13.	main lithology	granitoid	granite	magnetite	<1%	biotite	10-20%	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Very homogeneous pink granite  2.3 Ga? Containing a few minor xenoliths.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	South of the main granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1162-1	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1163	11-07-2023 13:30:51.981	59.809487	-110.151891	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	800	-9999	-9999	-9999	Hematized coarse grained to pegmatitic granite. Just past big area of gneiss. Measurements - Scint up to 800 cps.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	hematite red	massive	-9999	pegmatitic	Hematized. High cps.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	250	79	-9999	Banding that has been folded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1163-1	whole-rock lithogeochemistry	Hematized granite with high cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1164	11-07-2023 14:14:11.844	59.807411	-110.152531	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	4	-9999	-9999	-9999	400	-9999	-9999	-9999	Outcrop shows ductile flow with intrusion of pink granite. Measurements - Scint avg 400 cps; MS 4.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pale pink	gneissic	-9999	phaneritic coarse (5-10mm)	Folded and injected by younger granites.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1164-1	whole-rock lithogeochemistry	Gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1165	11-07-2023 14:44:38.928	59.807145	-110.154455	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	Contains a large amphibolite layer/pod as well as a few other random xenoliths. This granite extends westward towards the swamp. Looks to extend all the to the lake.	raft	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	black	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1165-1	whole-rock lithogeochemistry	Amphibolite sheet. Dismembered and discontinuous. Age relationship with granite is unclear but looks older. May be recrystallized to biotite rich.	AL-23-1165-2	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1166	13-07-2023 09:20:13.450	59.811978	-110.257620	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	50	300	-9999	400	-9999	-9999	-9999	Measurements - 300 to 400 cps.  MS up to 50.	main lithology	gneiss	orthogneiss	magnetite	<1%	-9999	-9999	-9999	-9999	pink and hematized	gneissic	-9999	-9999	Injected by granite. The gneiss is less than 50%.	main lithology	granitoid	granite	biotite	5-10%	chlorite	1-5%	-9999	-9999	hematite pink	foliated	-9999	phaneritic medium (1-5mm)	Approx. 60% of outcrop. Fairly leucocratic. Medium grained. Biotite may be replacing original hornblende.	FOL1 - Foliation gen1	238	51	Foliation strong	In the gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1166-1	whole-rock lithogeochemistry	Granitic component.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1167	13-07-2023 10:10:01.599	59.807711	-110.264527	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	1600	-9999	-9999	-9999	Scint up to 1600 cps along a structure.  Lots of magnetite. Moly was recorded by Godfrey, but none was found at this outcrop.	minor lithology	granitoid	quartz diorite	magnetite	<1%	hornblende	5-10%	biotite	10-20%	salt and pepper	foliated	equigranular	phaneritic medium (1-5mm)	This is a zone of salt and pepper granitoid that is more mafic. Most of the outcrop is a mix of pink granite and basement gneiss.	main lithology	granitoid	granite	magnetite	<1%	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	Measurements - Scint locally 1500 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1167-1	whole-rock lithogeochemistry	Diorite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1168	13-07-2023 11:12:29.898	59.815499	-110.267108	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	paragneiss	garnet	1-5%	sillimanite	<1%	biotite	10-20%	grey	gneissic	-9999	phaneritic medium (1-5mm)	Very hard quartz rich recrystalized garnet-biotite rock that contains pyrite and possibly some graphite. Mo was described here but does not exist.	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	pegmatitic	There are some pegmatitic sheets.	FOL1 - Foliation gen1	185	77	Foliation strong	Rock is very hard.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1168-1	whole-rock lithogeochemistry	Sediment with pyrite.	AL-23-1168-2	whole-rock lithogeochemistry; thin section	Garnet bearing zone.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1169	13-07-2023 11:36:44.919	59.821217	-110.298993	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.2	-9999	12	-9999	-9999	-9999	-9999	-9999	-9999	Middle of outcrop is metasediments and amphibolite. West and east side is basement complex. Metasediments are mag low (MS 0.2), but basement complex is mag high (MS 12).	main lithology	gneiss	paragneiss	biotite	20-50%	-9999	-9999	-9999	-9999	layered white and grey	-9999	-9999	-9999	Compositional layering and banding. Quartz rich layers. Amphibolite band 5 m wide.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Basement complex gneiss with younger pink granite.	FOL1 - Foliation gen1	20	78	Foliation strong	-9999	LINF - Lineation fold	205	65	-9999	Locally with S2.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1170	13-07-2023 13:58:55.852	59.815201	-110.205545	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.07	5	-9999	-9999	215	-9999	-9999	-9999	This is 300 m from dated location of 2.3 ga granite. Very homogeneous granite. 215 cps. MS 0.07 but there are a few spots that are 5+.  	main lithology	gneiss	granite	chlorite	1-5%	biotite	5-10%	-9999	-9999	pink to hematitic	foliated	equigranular	phaneritic coarse (5-10mm)	Very homogeneous 50 m of lichen rounded outcrops.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	240	78	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1170-1	whole-rock lithogeochemistry; thin section	This is prime granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1171	13-07-2023 14:12:57.290	59.814314	-110.205326	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	600	-9999	-9999	-9999	Nice big outcrops of the same granite as previous.  Measurements - Scint max 600 cps locally.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1171-1	whole-rock lithogeochemistry	2.3 Ga granite, but pegmatitic phase here. Lower mag then basement gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1172	13-07-2023 15:04:21.355	59.827926	-110.138051	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.2	-9999	-9999	-9999	1500	-9999	-9999	-9999	Huge outcrop area at the south of the island. Very homogeneous except for the level of strain. Measurements - MS 0.2; Up to 1500 cps locally. 	main lithology	granitoid	granite	biotite	5-10%	muscovite	1-5%	-9999	-9999	white to light pink	massive	-9999	phaneritic coarse (5-10mm)	Leucocratic, locally pegmatitic. Massive to moderately foliated. Rare Xenoliths and zones of vaguely gneissic material. Less deformed and coarser grained that the 2.3 Ga granite we just visited. Plus there is some Muscovite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	10	71	Foliation moderate	Massive to moderately strained and beaded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1172-1	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1173	13-07-2023 15:58:38.436	59.834686	-110.120739	Internal GPS	Russell Hartlaub	Russell Hartlaub	5	-9999	6	-9999	-9999	200	-9999	-9999	-9999	Big waves on the lake coming over here. MS 5 to 6.  Small epidote veins.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pale pink to buff	foliated	-9999	phaneritic coarse (5-10mm)	Same as on the previous outcrop. Homogeneous and moderately foliated granite. Some pegmatite parches. 200 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	155	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1174	13-07-2023 16:33:49.118	59.835567	-110.122190	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.4	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Climbed up the hill here. It’s a mix of basement gneiss with amphibolite intruded by the Colin lake granite.  MS 0.4.	main lithology	granitoid	granite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Contains large zones of gneiss.	main lithology	gneiss	orthogneiss	hornblende	5-10%	-9999	-9999	-9999	-9999	pale grey banded	gneissic	-9999	phaneritic coarse (5-10mm)	Layer parallel sheets of granite within the gneiss. Also amphibolite.	FOL1 - Foliation gen1	140	74	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1174-1	whole-rock lithogeochemistry	Granite from top of the hill. The granite here contains pegmatites that are variably folded.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1175	14-07-2023 09:36:18.900	59.794871	-110.196431	Internal GPS	Russell Hartlaub	Russell Hartlaub	4	-9999	20	-9999	280	500	-9999	-9999	-9999	Lichen covered. MS 4 to 20.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink hematized locally	gneissic	-9999	phaneritic medium (1-5mm)	Strongly recrystalized. Green chlorite replacing hornblende? Smeared.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	40	68	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1176	14-07-2023 09:53:27.882	59.793476	-110.197908	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	22	-9999	-9999	220	-9999	-9999	-9999	-9999	Measurements - MS 22;  Scint avg 220 cps.	main lithology	granitoid	granite	magnetite	<1%	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Beaded feldspars that are 1 to 3 mm. Recrystalized. Ribbon mylonite locally.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1176-1	whole-rock lithogeochemistry	Granite. Sample contains some plag? Phenocrysts that are black.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1177	14-07-2023 10:21:39.071	59.792694	-110.198899	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Pure granite all the way from last outcrop. Sheared locally but fairly clean with no pegmatites. Xenolith of gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	236	73	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1177-1	whole-rock lithogeochemistry; thin section	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1178	14-07-2023 10:44:24.382	59.792515	-110.200784	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	1	-9999	-9999	240	300	-9999	-9999	-9999	Measurements - MS 1; Scint avg 240 cps.	main lithology	granitoid	granite	biotite	5-10%	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Injecting the orthogneiss unit. It’s about 50% granite. Locally pegmatitic. Xenoliths.	minor lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink with banding	gneissic	-9999	-9999	Found as layers and rotated xenoliths in the granite. More magnetic.	FOL1 - Foliation gen1	200	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1179	14-07-2023 11:09:05.650	59.791780	-110.203088	Internal GPS	Russell Hartlaub	Russell Hartlaub	1	-9999	20	-9999	260	500	-9999	-9999	-9999	Nice big clean outcrop. Measurements - MS 1 to 20 (in a darker band); Scint avg 260 cps, 500 cps max along fractures.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	gneissic	-9999	phaneritic medium (1-5mm)	Injected by 40% granite.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Injecting the orthogneiss. Xenoliths and rotated and folded sheets are common. Locally pegmatitic.	FOL1 - Foliation gen1	248	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1180	14-07-2023 11:27:42.102	59.791446	-110.205170	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	35	-9999	-9999	-9999	220	-9999	-9999	-9999	Measurements - MS 35; Scint avg 220 cps.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey banded	gneissic	-9999	phaneritic medium (1-5mm)	Excellent grey gneiss. Oldest component in the area. There is also a small amount of pink granite sheet.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	268	60	-9999	Gneissic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1180-1	whole-rock lithogeochemistry; thin section	Big perfect gneiss sample. Geochron would be ideal.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1181	14-07-2023 12:23:36.341	59.792461	-110.209386	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	8	-9999	-9999	110	800	-9999	-9999	-9999	Huge black gabbro (amphibolite composition) outcrop. Homogenous with no banding or layers. MS 8. Scint low except at pegmatite.	main lithology	gabbroid	gabbro	hornblende	20-50%	plagioclase	20-50%	-9999	-9999	black	foliated	equigranular	phaneritic very coarse (10-50mm)	Contains a few small zones of pegmatite. Traces of sulfide.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white	-9999	-9999	pegmatitic	Pegmatite (50 cm thick). Disrupted.  Scint 800 cps. 068/80 for orientation.	FOL1 - Foliation gen1	165	78	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1181-1	whole-rock lithogeochemistry; thin section	Contains trace sulfide.	AL-23-1181-2	whole-rock lithogeochemistry	Pegmatite with 800 cps.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1182	14-07-2023 13:18:25.667	59.792090	-110.212450	Internal GPS	Russell Hartlaub	Russell Hartlaub	1	-9999	12	-9999	200	300	-9999	-9999	-9999	Measurements - MS 12 (for gneiss); MS <1 (for granite); Scint up to 300 cps.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Pink granite injecting and encompassing older grey gneiss. Locally pegmatite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey	-9999	-9999	-9999	Some biotite rich brown zones. Injected by granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1183	14-07-2023 13:50:34.236	59.793136	-110.214374	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	280	-9999	-9999	-9999	-9999	Huge clean outcrop. 3 components. 1 - grey gneiss. 2- mafic amphibolite. 3 - pink granite that intrudes both.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	phaneritic coarse (5-10mm)	Locally with deformed phenocrysts.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey and finely banded	gneissic	-9999	phaneritic medium (1-5mm)	Grey. May be associated with the big bands of amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1183-1	whole-rock lithogeochemistry	Amphibolite that is a sheet injected by the granite.	AL-23-1183-2	whole-rock lithogeochemistry	Pink leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1184	14-07-2023 14:17:12.940	59.794427	-110.211910	Internal GPS	Russell Hartlaub	Russell Hartlaub	1.3	-9999	25	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 25 (in gneiss); MS 1.3 (in granite).	main lithology	gneiss	orthogneiss	magnetite	<1%	-9999	-9999	-9999	-9999	grey	gneissic	-9999	-9999	Ghostly grey and brown banding that is injected by the granite.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink and hematitic in places	foliated	-9999	-9999	Injection.	LINF - Lineation fold	46	48	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1185	14-07-2023 15:04:41.995	59.794683	-110.209459	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	120	700	-9999	-9999	-9999	Large 100 m long outcrop area at top of hill that is all amphibolite gabbro. We passed through strongly folded grey gneiss on the way here. Quartz vein from previous station (LL-23-1084) extend to this station.	main lithology	gabbroid	gabbro	hornblende	20-50%	-9999	-9999	-9999	-9999	black	-9999	-9999	phaneritic very coarse (10-50mm)	Very homogeneous and coarse grained. Some quartz kspar veins and dikes.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1185-1	whole-rock lithogeochemistry	Gabbroic.	AL-23-1185-2	whole-rock lithogeochemistry; thin section	Gabbro.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1186	14-07-2023 15:28:37.691	59.794384	-110.202993	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	260	-9999	-9999	-9999	-9999	Small series of lichen covered outcrops. Measurements - MS variable; Scint avg  260 cps.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	We have seen this unit since the gabbro hill. Unit was sheared at contact with gabbro. Granodiorite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1187	15-07-2023 08:43:30.287	59.908304	-110.110903	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.01	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Fresh burned area.  Granite MS 0.01.	main lithology	granitoid	quartz monzonite	muscovite	1-5%	biotite	1-5%	-9999	-9999	white to pink	foliated	-9999	phaneritic very coarse (10-50mm)	Quartz poor here. Traces of Muscovite. Leucocratic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	240	70	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1187-1	whole-rock lithogeochemistry; thin section	Pegmatitic component.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1188	15-07-2023 09:33:51.457	59.937189	-110.129861	Internal GPS	Russell Hartlaub	Russell Hartlaub	3	-9999	5	-9999	-9999	-9999	-9999	-9999	-9999	Major shear zone here. Looks like we can link it up with some of the Godfrey shears. This lies along the major magnetic break that you see though here.  Measurements - MS 3 to 5.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Banded with pophyroclasts. Original rock is likely granitic. Hematitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	215	54	Foliation intense	Mylonite. This banding has been folded slightly.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1188-1	whole-rock lithogeochemistry; thin section	Mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1189	15-07-2023 10:30:25.403	59.941092	-110.125956	Internal GPS	Russell Hartlaub	Russell Hartlaub	4	-9999	6	-9999	250	600	-9999	-9999	-9999	Measurements - MS 4 to 6; Scint 250 cps locally, up to 600 cps in pegmatite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey with darker layers in the gneiss	gneissic	-9999	phaneritic medium (1-5mm)	Lots of folds here. Gneissic bands vary in thickness up to 20cm. Cut by the pegmatite dikes.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	pegmatitic	Pegmatite that cuts foliation.	FOL1 - Foliation gen1	230	57	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1189-1	whole-rock lithogeochemistry	Pegmatite.	AL-23-1189-2	whole-rock lithogeochemistry; thin section	Basement gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1190	15-07-2023 11:13:18.538	59.952810	-110.078878	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.01	-9999	300	-9999	970	-9999	-9999	-9999	Measurements - MS 0.01; Scint 300-600 cps,  970 cps on a pegmatitic patch.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white	foliated	equigranular	phaneritic very coarse (10-50mm)	Leucocratic white granite. MS - 0.01. Xenoliths of schist in the granite. Locally pegmatite.	minor lithology	schist	felsic schist	biotite	10-20%	-9999	-9999	-9999	-9999	grey and rusty	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	195	57	-9999	Schist. No structure recorded in granite.	SH - Shear Ductile	335	70	-9999	Shear zone cutting through the outcrop.	-9999	-9999	-9999	-9999	-9999	AL-23-1190-1	whole-rock lithogeochemistry; thin section	Schist. 	AL-23-1190-2	whole-rock lithogeochemistry; thin section	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1191	15-07-2023 12:24:03.386	59.961374	-110.078533	Internal GPS	Russell Hartlaub	Russell Hartlaub	0.16	-9999	0.3	-9999	-9999	-9999	-9999	-9999	-9999	Schistose paragneiss injected by pegmatite. And deformed. Measurements - MS 0.16 to 0.3.	main lithology	gneiss	paragneiss	biotite	10-20%	-9999	-9999	-9999	-9999	grey and rusty	layered	-9999	phaneritic medium (1-5mm)	Good compositional layering.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	220	38	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1191-1	whole-rock lithogeochemistry; thin section	Rusty schist layer. Sillimanite? More pelitic.	AL-23-1191-2	whole-rock lithogeochemistry; thin section	Quartz rich layer. Quartzite?	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1192	15-07-2023 13:54:48.251	59.965028	-110.077843	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Old showing area. Looking for signs of copper. Measurements - MS 0.15.	main lithology	schist	intermediate schist	biotite	20-50%	-9999	-9999	-9999	-9999	rusty	schistose	-9999	-9999	Zones of schist intermixed with chewed up granite. There is also quartz rich zones that could potentially be quartzite.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink and beaded	-9999	-9999	-9999	Sheared up granite.	FOL1 - Foliation gen1	155	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1192-1	whole-rock lithogeochemistry	Schist. Very dark.	AL-23-1192-2	whole-rock lithogeochemistry	Heavily altered granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1193	15-07-2023 14:16:34.235	59.965608	-110.076824	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Sillimanite (?).	main lithology	gneiss	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	rusty	-9999	-9999	-9999	Quartz rich. Good compositional layering. Quartz rich. Lots of folding.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	5	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1193-1	whole-rock lithogeochemistry; thin section	Paragneiss with Sillimanite? Graphite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1194	15-07-2023 14:43:32.686	59.964005	-110.076176	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Biotite schist. Likely a sedimentary rock that has been sheared. There is also injected granite.	main lithology	schist	felsic schist	biotite	20-50%	-9999	-9999	-9999	-9999	grey with lots of black lichen	schistose	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	200	74	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1195	15-07-2023 15:24:33.804	59.940161	-110.042273	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.12	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Andrew lake granodiorite. Big fault structure that runs down this side of the valley. Add to the map.  There is a scarp along this side of the bay.  Fault parallel to Bonny. MS 0.12.  	main lithology	granitoid	granodiorite	alkali-feldspar	20-50%	-9999	-9999	-9999	-9999	buff	massive	porphyritic	phaneritic coarse (5-10mm)	Very distinctive. Locally hematized. Phenocrysts are randomly oriented. Huge outcrop area that runs up to the fault/cliff. One small (20 cm) rounded xenolith of mafic material.	dike	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	massive	-9999	pegmatitic	Inter growth of quartz and kspar. No mafic minerals.	FOL1 - Foliation gen1	181	85	Foliation moderate	Local zone of strong flattening. Much of the granite is only weakly foliated.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1195-1	whole-rock lithogeochemistry; thin section	Granodiorite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1196	16-07-2023 09:30:19.675	59.815521	-110.135592	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz flooding along this intrusive contact between the white granite and the metasediments.	main lithology	gneiss	paragneiss	sillimanite	<1%	-9999	-9999	-9999	-9999	brown to grey	gneissic	-9999	phaneritic medium (1-5mm)	Compositional layering in the meta sediments. There are NO porphyroclasts, or other evidence that this unit is tectonic. Best interpretation is a quartz rich sediment, likely a sandstone with some more quartz rich layers. No garnet here, but brown knots of what look to be folded sillimanite. Get TS. Lots of folding.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white	-9999	-9999	-9999	Leucocratic quartz flooded intrusive boundary.  This is the Colin Lake granite. Quartz flooding here may be caused by dewatering of the sediment. Rafts and blocks of sediment are also entrained in the granite. The red hematized granite does not have xenol	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1196-1	whole-rock lithogeochemistry; thin section	Banded metasediments.	AL-23-1196-2	whole-rock lithogeochemistry; thin section	Nice folded sediment with lots of possible sillimanite knots.  Big sample.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1197	16-07-2023 10:11:51.033	59.814621	-110.137746	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Boundary between red hematized porphyry granite in east with orthogneiss in west. Boundary looks tectonic.  Gneiss is also injected by granite and pegmatite.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey banded	gneissic	-9999	-9999	Biotite rich gneiss. Tectonized to the west with some dismembered porphyroclasts pegmatite dike cuts gneiss.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink hematitic	massive	porphyritic	phaneritic coarse (5-10mm)	Weak level of foliation suggests it is Taltson aged.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1198	16-07-2023 11:38:01.398	59.816750	-110.153367	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink, hematized	foliated	-9999	phaneritic coarse (5-10mm)	Very highly foliated, sheared and folded pink granite. Foliation here bends to nearly perpendicular the surrounding area. Typical Uranium City type.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	140	71	Foliation intense	High strain zone bends here.	LINF - Lineation fold	158	52	-9999	S folds.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1199	16-07-2023 11:54:36.196	59.816349	-110.156147	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	All granitic right up to the end of this outcrop.	main lithology	granitoid	granite	biotite	5-10%	chlorite	1-5%	-9999	-9999	pink, hematized	foliated	-9999	-9999	The south end of the outcrop is strong tectonized with some quartz veining. Looks like possible gneiss injected by granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	SH - Shear Ductile	118	84	-9999	Shear with quartz veins.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1199-1	whole-rock lithogeochemistry	Granitic injection into some gneissic material at end of outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1200	16-07-2023 14:45:06.766	59.872179	-110.122346	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.02	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.02	main lithology	granitoid	granite	garnet	1-5%	-9999	-9999	-9999	-9999	white	foliated	-9999	phaneritic coarse (5-10mm)	Weakly foliated. Clean white leucogranite with garnet.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	285	74	Foliation weak	Looks more like a set of discrete shears that are flattening.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1200-1	whole-rock lithogeochemistry	White leucogranite with garnet.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1201	16-07-2023 15:14:47.668	59.878077	-110.119568	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.01	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strong ribbon mylonite of granite in places. Locally coarse grained. Measurements - MS 0.01.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	white to pink	foliated	-9999	phaneritic coarse (5-10mm)	Mylonitic, locally ribbon mylonite and schistose mylonite. Looks to be the same leucogranite as in the previous station, but very highly strained and including mylonite xenoliths of possible sediments.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	SH - Shear Ductile	235	70	-9999	Mylonitic fabric.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1201-1	whole-rock lithogeochemistry; thin section	Relatively undeformed part of the outcrop. Leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1202	16-07-2023 15:54:20.035	59.869330	-110.089742	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Striking weathering along the beach.  Looks more mafic, perhaps due to weathering of the ground mass. Right up the hill in lichen covered area it looks like the Colin Lake white leucogranite.	main lithology	mylonite	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	white to gray at water	foliated	porphyritic	phaneritic very coarse (10-50mm)	Cut by numerous white pegmatites. Highly strained and Mylonitic in part. Up from the shore you lose the phenocrysts into the Colin Lake granitoid?	dike	mylonite	granite	-9999	-9999	-9999	-9999	-9999	-9999	white weathering pegmatite sheets.	-9999	-9999	-9999	The white pegmatites make up 20% of the outcrop. We sampled a large one that’s at least 10 m wide and extends up the hill.	FOL1 - Foliation gen1	265	59	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1202-1	whole-rock lithogeochemistry	Pegmatite that cuts the Andrew Lake granodiorite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1203	16-07-2023 16:57:57.441	59.849796	-110.098586	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.14	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Measurements - MS 0.14.	main lithology	granitoid	granodiorite	biotite	10-20%	hornblende	1-5%	-9999	-9999	pink	-9999	porphyritic	phaneritic coarse (5-10mm)	Relict hornblende.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1203-1	whole-rock lithogeochemistry	Grungy sample needs to be cut.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1204	17-07-2023 13:45:07.700	59.895607	-110.066959	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Nice homogeneous granite. White to pink. Measurements - MS 0.00	main lithology	granitoid	granite	muscovite	1-5%	biotite	1-5%	-9999	-9999	-9999	-9999	-9999	phaneritic coarse (5-10mm)	Lots of boulders here on top of outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	330	37	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1204-1	whole-rock lithogeochemistry	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-1205	17-07-2023 14:07:58.069	59.904705	-110.066833	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.16	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Composition is homogeneous on north side of island. No layering or xenoliths. MS 0.16.	main lithology	dioritoid	quartz diorite	biotite	10-20%	hornblende	5-10%	-9999	-9999	grey uniform with white quartz veins	foliated	equigranular	phaneritic medium (1-5mm)	Best guess is that this is an intermediate intrusive rock. There is a bit melt looking patches indicating upper amphibolite as a probable grade. Injected by numerous pegmatites and granite especially at the south end of the island.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-1205-1	whole-rock lithogeochemistry	Dioritic component. Biotite rich.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2065	04-07-2023 16:42:26.690	59.843544	-110.111945	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	300	-9999	500	-9999	-9999	-9999	Colin granite, to the east we start seeing transitional contact? With potential metaseds. Granite background is 500 cps, 300 cps is potential slivers of metaseds, which are cut by Colin granite. Leucogranite melt to the west becomes coarser, more pegmatitic and cross cut the biotite schist (lith 2 and the foliation taken from the schist).	main lithology	granitoid	granite	biotite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	unknown	schist	intermediate schist	biotite	20-50%	quartz	10-20%	muscovite	10-20%	black to dark grey	layered	equigranular	phaneritic fine (0.5-1mm)	Very micaceous sheen, observed in slivers and patches moving west up to 4 m wide. MS 0.02 to 0.2 in the leucogranite. Very clearly intruding the biotite schist.	FOL - Foliation	11	90	Foliation moderate	Found in slivers of metaseds.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2065-1	whole-rock lithogeochemistry	Colin Lake leucogranite.	AL-23-2065-2	whole-rock lithogeochemistry	Biotite schist.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2066	05-07-2023 09:26:06.088	59.838970	-110.151401	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	330	-9999	504	-9999	-9999	-9999	Measurements - cps 330 to 504.	main lithology	granitoid	granite	biotite	10-20%	alkali-feldspar	20-50%	plagioclase	10-20%	buff	massive	equigranular-xenomorphic	phaneritic medium (1-5mm)	Quartz and alkali feldspar (perthite) pegmatite melt (rare, localized), moderate hematite staining.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	227	88	Foliation weak	Anastomosing. Measurement taken at shoreline.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2066-1	whole-rock lithogeochemistry	Granite, higher up on outcrop, 10-15 m west from shoreline, more massive.	AL-23-2066-2	whole-rock lithogeochemistry; thin section	Granite at shoreline, stronger foliation, starting to show segregation of felsic and mafic minerals, verging on gneissic banding. Same mineral composition as sample 1. Rare localized quartz veins.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2067	05-07-2023 10:16:01.337	59.839565	-110.144656	Internal GPS	Calla Knudson	Nicholas Montenegro	-9999	-9999	-9999	178	-9999	243	-9999	-9999	-9999	Island.  Measurements - 178-243 cps.	main lithology	granitoid	granite	quartz	20-50%	alkali-feldspar	20-50%	biotite	1-5%	cream to buff	foliated	porphyritic	phaneritic medium (1-5mm)	Medium to coarse grained; biotite altering to yellowish green chlorite stringers, local layer parallel qtz melts. On western side of island, main lithology becomes slightly coarser and a bit more foliated to the west. Local cataclastic brecciation, and qtz K-spar melts. Probable white Muscovite, very powdery.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	220	90	Foliation moderate	Eastern side of island.	FOL - Foliation	231	90	Foliation strong	Western point of island.	-9999	-9999	-9999	-9999	-9999	AL-23-2067-1	whole-rock lithogeochemistry	Granite with potential muscovite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2068	05-07-2023 11:26:17.963	59.849487	-110.143756	Internal GPS	Calla Knudson	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mafic enclave, irregular, gritty quartzofeldspathic fine grained component, enveloped by biotite. Quartz and feldspar pegmatitic melt. Garnetiferous leucogranite.	main lithology	gneiss	granite	muscovite	5-10%	garnet	1-5%	alkali-feldspar	20-50%	cream	gneissic	porphyritic	phaneritic coarse (5-10mm)	Verging on gneissic (unclear). 1-5% biotite, 1-5% garnet. Muscovite has yellowish green alteration (chlorite.). Quartz is smoky. Coarse to very coarse grained. Melt patches, biotite-rich, potential paleosome, containing sillimanite and garnet (partial melting?).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	245	30	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2068-1	whole-rock lithogeochemistry; thin section	Garnetiferous Colin Lake leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2069	05-07-2023 12:32:48.384	59.851913	-110.146290	Internal GPS	Calla Knudson	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	5.3	11.8	5.3	Protomylonite, seeing sheared and foliation wrapped porphyroclasts of quartzofeldspatchic material up to 10 cm in width and length. UTM 0547898 E 6635044 N. Colin Lake leucogranite with rafts of mylonitic paragneiss. Scintillometer assay: U = 19 ppm, DR = 247.2 nSvh-1, K = 5.3%, Th = 11.8 ppm (from cliff exposure with mild to moderate yellow staining). 	main lithology	mylonite	granite	quartz	20-50%	alkali-feldspar	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	raft	gneiss	paragneiss	garnet	1-5%	biotite	-9999	sillimanite	1-5%	-9999	-9999	-9999	-9999	Biotite- and possibly sillimanite-bearing; potential raft of paragneiss preserved on the margins of Colin Lake leucogranite.	FT - Fault Brittle	232	90	-9999	In L1 outcrop up slope from shore.	FOL - Foliation	230	90	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2069-1	whole-rock lithogeochemistry	At shoreline, possible metasediments, L2.	AL-23-2069-2	whole-rock lithogeochemistry	At outcrop with fault, main lith (granite) with yellow staining.	AL-23-2069-3	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2070	05-07-2023 13:45:11.016	59.851055	-110.147221	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	700	-9999	-9999	-9999	Pink weathering, highly strained, mylonititic/recrystallized biotite gneissic granite. Mesoscopic folding well exposed and pervasive. Scint 700 cps background. Quartz perthite pegmatite coming in along axial fold planes. Migmatitic, with melt in-situ melt patches. Local and rare rafts of garnet bearing paragneiss to the east, along the mylonite zone.	main lithology	mylonite	granite	alkali-feldspar	20-50%	biotite	20-50%	garnet	1-5%	buff	gneissic	equigranular	phaneritic medium (1-5mm)	Pegmatite coming in parallel to fold axial planes; gneissic pink and black banding on fresh surface.	raft	gneiss	paragneiss	garnet	1-5%	biotite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	AXF - Axial fold plane	79	90	-9999	Hinge line orientation is 62-260.	AXF - Axial fold plane	264	90	-9999	Hinge line 72-262.	FOL1 - Foliation gen1	214	69	Foliation intense	-9999	AL-23-2070-1	whole-rock lithogeochemistry	Granite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2071	05-07-2023 14:47:19.266	59.851250	-110.148876	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Highly strained, gneissic biotite granite, folded with m-scale lenses of amphibolite, m- to c-grained. Calla's notes: 198/90: foliation; pegmatite layer parallel; possible cordierite in dark unit.	main lithology	mylonite	granite	alkali-feldspar	20-50%	biotite	20-50%	quartz	10-20%	buff	gneissic	equigranular	phaneritic medium (1-5mm)	Both the granite gneiss and the amphibolites are folded, resulting in pinching out of amphibolite lenses.	enclave	mafic rocks	amphibolite	hornblende	20-50%	plagioclase	20-50%	biotite	20-50%	dark grey to black	foliated	porphyritic	phaneritic medium (1-5mm)	No notes captured.	AXF - Axial fold plane	337	78	-9999	Hinge line.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2071-1	whole-rock lithogeochemistry	Amphibolite.	AL-23-2071-2	whole-rock lithogeochemistry	Granite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2072	05-07-2023 15:47:05.913	59.854540	-110.130145	Internal GPS	Calla Knudson	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Leucogranite, locally garnetiferous; local mini shear zones. Featuring rafts of potential paragneiss, with folded fabric, which appear melted and could represent a paleosome to the leucogranite.	main lithology	granitoid	granite	quartz	10-20%	feldspar	20-50%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2072-1	whole-rock lithogeochemistry	Lith 1 (leucogranite - locally garnetiferous).	AL-23-2072-2	whole-rock lithogeochemistry; thin section	Rusty potential metaseds.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2073	06-07-2023 09:50:22.183	59.829295	-110.301269	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	90	5000	-9999	-9999	-9999	Background cps ~90; overall biotite granite gneiss, with m-scale rafts of potential metasediments reaching up to 5000 cps on scintillometer (see lith 2 notes). Calla's notes: Lith 2: chlorite biotite schist, rusty, with porphyroclasts of feldspar and quartz, possible cordierite. Lith 1: leucogranite (qtz +feldspar), yellow gold-coloured alteration, metallic mineral disseminated throughout, flecks of pyrite (?), very hematized, 20-50% qtz, 20-50% feldspar, trace garnet, waxy texture; layer parallel pegmatite and quartz melt; discontinuous beds of lith 2 moving westward, whole outcrop may represent gradational contact of colin leucogranite w/ potential metaseds.	main lithology	gneiss	granite	alkali-feldspar	20-50%	-9999	-9999	-9999	-9999	buff to dark grey	foliated	porphyritic	phaneritic medium (1-5mm)	Mainly not hot k spar granite, 400 cps (Sample 1), with rare layers of biotite schist, (not hot compared to radioactive pelite rafts (Sample 3)) and local pegmatite melt with perthite and albite. Gneissic and mylonitic, with local massive granite. Lith 2 is in contact with hot granite on its eastern margin, (up to 3-4000 cps/ sample 2).	raft	schist	intermediate schist	sillimanite	1-5%	biotite	20-50%	feldspar	10-20%	dark grey	schistose	-9999	phaneritic fine (0.5-1mm)	Significant amount of qtz and feldspar in fine grained pelitic to psammopelitic matrix, gritty and grains are not interlocking. Porphrycoclasts of feldspar and qtz of medium to coarse grained size, in addition to sheared, conglomeratic clasts of feldspar 	IGC - Contacts	70	70	Foliation strong	Contact between conglomeratic biotite pelite and hot, alkali feldspar granite.	FOL - Foliation	34	83	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2073-1	whole-rock lithogeochemistry	Not hot, host granite (western side of outcrop).	AL-23-2073-2	whole-rock lithogeochemistry	Hot granite in contact with lith 2.	AL-23-2073-3	whole-rock lithogeochemistry	Pelite raft.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2074	06-07-2023 10:52:13.634	59.829092	-110.302991	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Just moved through a gradational contact between the mylonite granite gneiss, where we saw consistent interlayering of the biotite schist and the granite, west  into clear layers of compositionally banded garnetiferous sediments. Melt of quartz and feldspar.	main lithology	metatexite	paragneiss	garnet	5-10%	sillimanite	1-5%	biotite	10-20%	dark grey to dusty brown	layered	porphyritic	phaneritic fine (0.5-1mm)	Well banded biotite schist with compositional layering of more pelitic schist alternating with psammopelitic layers concentrated with garnet in a fine grained matrix of biotite, feldspar, and grains. No interlocking texture and all layers are sillimanite bearing, though more pronounced in psammopelitic layers. Possible cordierite and probable chlorite overprint. Biotite retrograding from hornblende, and the matrix is strongly magnetic but sporadically, detrital magnetite or chalcopyrite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	IGC - Contacts	34	90	-9999	-9999	FOL - Foliation	29	89	Foliation intense	Mylonitic foliation, anastomosing around vertical.	-9999	-9999	-9999	-9999	-9999	AL-23-2074-1	whole-rock lithogeochemistry; thin section	Garnetiferous psammopelite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2075	06-07-2023 11:38:42.796	59.827898	-110.306889	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	300	390	-9999	-9999	-9999	Into full on metasediments, with alternating pelitic and psammopelitic layers, very highly strained/mesomylonitic and intruded by fine grained, layer parallel aplite dikes; granitic porphyroclasts are wrapped by the foliation.  To the east, there is. 3 m wide layer of sil-bio schist, dark black weathering. Layer parallel qtz melt and rare pegmatite melt. Measurements - 390 cps at sample site 1, general background of 300.	main lithology	metatexite	paragneiss	garnet	5-10%	feldspar	10-20%	biotite	10-20%	grey to buff	gneissic	porphyritic	phaneritic medium (1-5mm)	Seeing interlaying of pelite to psammite, the coarser layers more obviously garnet bearing up to 1cm. They are also smeared and sheared along the foliation into compositional layers. Finer grained pelite shows sillimanite and qtz, feldspar, biotite fine grained matrix.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	239	90	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2075-1	whole-rock lithogeochemistry; thin section	Psammopelitic garnetiferous layer of seds.	AL-23-2075-2	whole-rock lithogeochemistry; thin section	Rusty, gossanous metasediments, locally interlayered with the paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2076	06-07-2023 12:16:07.159	59.827944	-110.308668	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	metatexite	paragneiss	garnet	5-10%	-9999	10-20%	feldspar	20-50%	light grey	gneissic	porphyritic	phaneritic coarse (5-10mm)	Psammitic component of paragneiss, with cm-scale, relatively intact garnets which are clearly retrograding to biotite in a medium to coarse grained matrix of feldspar, quartz, and biotite. Main lithology is sample 2.	minor lithology	schist	intermediate schist	biotite	10-20%	-9999	-9999	-9999	-9999	black	schistose	equigranular-idiomorphic	phaneritic fine (0.5-1mm)	Rusty, gossanous pelite to psammopelite, with an abundance of sulphides, (pyrite, chalcopyrite?). Sample 1 - very magnetic.	FOL - Foliation	223	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2076-1	whole-rock lithogeochemistry	Rusty gossan from lith 2 (pelite to psammopelite).	AL-23-2076-2	whole-rock lithogeochemistry; thin section	Main lith,  garnetiferous psammite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2077	06-07-2023 13:04:00.093	59.827383	-110.310353	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Gneissic and migmatitic, layered pelite to psammite with intermixed biotite sillimanite schist. Garnets up to 2-3cm wide, abundant; hematitezed layers of various grain sizes and rusty, sulphide rich quartz associated with the leucogranite. Seeing quartz tourmaline veins. Sample AL-23-2077-3 is Rusty quartz. Qtz parallel to fol and potentially axial planar to F2. Axial planar, 2nd gen foliation associated with folds 100 m to the south west, folds become oriented more towards 050/90.	main lithology	metatexite	paragneiss	garnet	5-10%	-9999	-9999	-9999	-9999	light grey to dusty tan	gneissic	porphyritic	-9999	Intruded by felsic leucogranitic injections and further folded with them; could this represent leucocratic neosome melting out of the Rutledge River complex? i.e. Colin Lake granitoids.	neosome	granitoid	granite	quartz	20-50%	feldspar	20-50%	-9999	-9999	cream	massive	migmatitic	phaneritic coarse (5-10mm)	No notes captured.	FOL - Foliation	220	82	Foliation strong	Anastomosing and folded,	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	26	79	Foliation moderate	-9999	AL-23-2077-1	whole-rock lithogeochemistry	Rusty gossanous paragneiss, finer grained than sample 2 and less leucosome.	AL-23-2077-2	whole-rock lithogeochemistry; thin section	Coarser grained paragneiss with more qtz leucosome melt.	AL-23-2077-3	whole-rock lithogeochemistry	Rusty quartz, parallel to foliation and potentially axial planar to F2.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2078	06-07-2023 14:16:12.201	59.827009	-110.314143	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Similar migmatitic paragneiss as previous station; rhythmically layered pelite to psammite; however, intruded by cream to buff weathering leucogranite and subsequently folded with it. They appear associated, in that the leucogranite may represent leucogranitic neosome melting out of the paragneiss, which is highly strained.	main lithology	metatexite	paragneiss	garnet	5-10%	-9999	-9999	-9999	-9999	light grey	gneissic	porphyritic	phaneritic medium (1-5mm)	Fine to medium grained, with layer parallel fine grained leucosome.	neosome	granitoid	granite	alkali-feldspar	20-50%	quartz	20-50%	-9999	-9999	cream to buff	foliated	porphyritic	phaneritic coarse (5-10mm)	Leucogranite, small amounts of mafic, dark coloured yet sometimes translucent minerals, qtz or plag could be bio or hornblende, less than 5 percent.	FOL - Foliation	185	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2078-1	whole-rock lithogeochemistry	Granitic leucosome.	AL-23-2078-2	whole-rock lithogeochemistry; thin section	Rusty garnetiferous pelite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2079	06-07-2023 14:38:43.750	59.826790	-110.315508	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Getting back into transitional contact, like we saw on eastern side. Interlayered biotite sil schist and fine to medium grained, leucosomal granite.	main lithology	metatexite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	buff to grey	gneissic	migmatitic	-9999	No notes captured.	neosome	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	buff	foliated	porphyritic	phaneritic medium (1-5mm)	Locally massive, becoming more dominant versus remnants of sediments (lith 1).	AXF - Axial fold plane	33	78	Foliation intense	71->210: hinge line.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2080	06-07-2023 15:32:14.228	59.828223	-110.323508	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	2300	-9999	-9999	-9999	-9999	-9999	-9999	Full on diatexite migmatite; 20x40 cm schlieren of mylonitized, quartzofeldspathic, biotite phyllonite suspended in pegmatitic leucosomal melt. Paleosome schlieren may reflect different sources (i.e., one schlieren is extremely well layered and may represent a volcaniclastic sediment, while others are more massive and coarse grained, reflecting more of a classic amphibolite). The sinistral shearing given by the schlieren conforms to the S-folding observed up until this point. Bayonet Lake shear zone sinistral?	main lithology	diatexite	diatexite	biotite	>50%	sillimanite	5-10%	-9999	-9999	black	layered	equigranular-idiomorphic	phaneritic fine (0.5-1mm)	Full on migmatite, schlieren of quartzofeldspathic, biotite phyllonite suspended in pegmatitic melt; rhythmically layered (compositional layering of clay and silt sized grains) pelitic verging on psammopelitic in layers; looks volcanic on weathered surface; mm-scale qtz and feldspar ribbons. Folded, and subsequently sheared in a brittle-ductile manner; hot pegmatite potentially coming in along axial planes during shearing, with sinistral offset; probable that the intruding, pebbly and apparently brecciated pegmatite displaced pieces of the schist, despite the schlierens of biotite phyllonite being completely suspended within pegmatitic melt with varying foliations up 20x40cm.	main lithology	neosome	pegmatite dike	alkali-feldspar	20-50%	biotite	20-50%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2080-1	whole-rock lithogeochemistry; thin section	Volcaniclastic schlieren (quartzofeldspathic, biotite phyllonite suspended in pegmatitic melt).	AL-23-2080-2	whole-rock lithogeochemistry	Layered granite and biotite schist, migmatitic, up to 2300 cps, clearly associated with pegmatite selvage.	AL-23-2080-2A	whole-rock lithogeochemistry	Additional hot/radioactive pegmatite.	AL-23-2080-3	whole-rock lithogeochemistry	Potential mylonitic paleosome, orthogneiss?	Alberta Geological Survey
AL-23-2081	07-07-2023 08:52:54.772	59.834205	-110.153395	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	730	-9999	-9999	-9999	Up the hill, seeing mesoscopic folds of ribbon mylonite, alkali feldspar granite making up granite component, and bio sillimanite(?) schist, making up mafic bands in the gneiss. Layer parallel pegmatite melt, with lots of biotite and quartz. Hitting max cps of 730 in granitic component. Porphyroclasts of granitic material wrapped up in biotite schist along foliation.	main lithology	mylonite	granite	sillimanite	1-5%	biotite	5-10%	alkali-feldspar	20-50%	pink	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Pink and dark grey gneiss; mylonitized granite with interlayers of biotite sillimanite(?)/chlorite schist, providing minerals for the mafic banding in the gneiss. Sample 2081-3 is pure schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	196	89	Foliation intense	Mylonitized, with folds.	AXF - Axial fold plane	31	90	-9999	First set of folds.	AXF - Axial fold plane	275	90	-9999	Second set of folds; 83->275; potential type 3 via F2 on F1?	AL-23-2081-1	whole-rock lithogeochemistry	Mylonitic granite.	AL-23-2081-2	whole-rock lithogeochemistry	Pegmatite contact with biotite schist.	AL-23-2081-3	whole-rock lithogeochemistry	Pure biotite schist.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2082	07-07-2023 09:55:37.332	59.831620	-110.162193	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Second of the day. Down by the water, we see transition from k spar granite on the east into full on mylonite, with layered leucosome up to 10cm in width which are boudinaged and sheared, anastomosing. Large chunks of quartzofeldspathic material, verging on pegmatitic grain size, quarts vein and half meter wide aplite  dikes cross cutting the mylonite in the orientation of 100 azimuth. Pebbly, brecciated pegmatite tends to be layer parallel.  Probably seeing ripped up chunks of the granite gneiss to the east. Matrix far out weighs the granitic component in the water. dike of aplite coming in axial planar to crenellations of, main fabric.	main lithology	gneiss	granite	alkali-feldspar	>50%	biotite	1-5%	quartz	10-20%	reddish pink	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Mostly alkali feldspar granite gneiss, moving east, roughly 20m, we start seeing inter layers of biotite sillimanite schist.	raft	schist	phyllonite	sillimanite	1-5%	biotite	>50%	muscovite	1-5%	dark grey to black	schistose	porphyritic	phaneritic very fine (0.1-0.5mm)	Tiny porphyroclasts of feldspar caught up in extremely biotite rich, micaceous matrix.	FOL - Foliation	41	83	Foliation strong	Increasingly mylonitized to the west across strike. Where we start seeing mylonitized granite, we see rafts and mm-scale inter layers of the schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2082-1	whole-rock lithogeochemistry	Alkali feldspar granite.	AL-23-2082-2	whole-rock lithogeochemistry; thin section	Schisty phyllonite, bio sillimanite and muscovite. Sillimanite may have been mistaken for chlorite in this case, not sure.	AL-23-2082-3	whole-rock lithogeochemistry	Mylonite component.	AL-23-2082-2A	whole-rock lithogeochemistry	Additional hot pegmatite.	Alberta Geological Survey
AL-23-2083	07-07-2023 10:58:08.058	59.826768	-110.160415	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Seeing mylonitized gneiss with mafic, biotite chlorite sillimanite(?) schist interlayers and quartzofeldspathic, white to buff weathering layers down by the water. It may reflect mylonitized paragneiss. The foliation bends in a clockwise manner on an axis cantered on a m-scale intrusion of k spar granite coming from the west. Granite probably nosing into hinges of major folds, and getting mixed up into the biotite schist during shearing/melting. Ribbon mylonite, ribboned ate and feldspar inter layered with mm scale laminate of bio sil mafic component of orthogneiss. Increasing felsic content moving west with increasing slope relief (Increasing elevation).	main lithology	gneiss	mesomylonite	chlorite	10-20%	biotite	>50%	quartz	5-10%	dark grey to black alternating to white to pink	gneissic	equigranular	phaneritic fine (0.5-1mm)	Felsic bands are coarser grained (med) vs the very fine grain size of the mafic layers. This stuff is bending around a large intrusion of granite gneiss, which could be deflecting foliation, or potentially nosing into folds during deformation. Phyllonitic within the fine grained mafic layers, which are abundant in micas, and sulfides (pyritic) cordierite? Alternating with white to pink weathering, quartzofeldspathic bands.	minor lithology	gneiss	alkali-feldspar granite	alkali-feldspar	>50%	biotite	5-10%	quartz	10-20%	pink to buff cream	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Much more k spar in this.	FOL - Foliation	300	80	-9999	Bends to 240 within a meter, and then to 261/56 moving back east around the granite intrusion.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2083-1	whole-rock lithogeochemistry	Alkali feldspar granite.	AL-23-2083-2	whole-rock lithogeochemistry	Unsubdivided mylonitic gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2084	07-07-2023 11:58:20.808	59.821511	-110.165593	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mostly alkali feldspar granite gneiss, intensely hematized and with rafts of biotite sil schist no larger than 10cm wide and a few feet in length.  Massive outcrop, covered mostly to the east, where the slope begins to decrease, seeing an increase in the abundance of biotite and width of mafic bands (30cm) which make up the grey component of the gneiss.  Whereas to the west, mostly dominated by Kspar granite, less interlayers of schist.	main lithology	gneiss	granite	alkali-feldspar	>50%	biotite	10-20%	quartz	5-10%	reddish pink	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Features sheared, rusty layers no greater than 10-20cm in width which are chlorite +/- sillimanite bearing. Crosscut by pegmatite veins and melts which are slightly oblique to general foliation and comprise pegmatitic grains of quartz and kspar wrapped up in extremely fine grained biotite rich matrix. Gneissic fabric is not very obvious; generally there are mm-scale layers of kspar and quartz alternating with biotite rich mafic bands. I think Im seeing muscovite along with potential metallic minerals (extremely fine grained sulfides). Amphibolite enclaves and lenses more common to the east.	minor lithology	granitoid	pegmatite dike	biotite	20-50%	alkali-feldspar	20-50%	quartz	10-20%	cream to buff	schistose	porphyritic	pegmatitic	Extremely fine grained biotite matrix with porphyroclasts of pegmatites of qtz and k spar. Pegmatite melts may include albite, perhaps perthite?	FOL - Foliation	159	84	Foliation weak	Weak, granite is locally massive and increasingly so to the west, away from the shearing. Becomes more clearly layered and gneissic to the east.	VN - Vein	190	76	-9999	Pegmatitic veins and melt in this orientatiom, slightly oblique to S-main.	-9999	-9999	-9999	-9999	-9999	AL-23-2084-1	whole-rock lithogeochemistry	Alkali feldspar granite.	AL-23-2084-2	whole-rock lithogeochemistry; thin section	Schist interlayer.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2085	07-07-2023 13:22:07.455	59.820119	-110.170999	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pink and grey gneiss; quartzofeldspathic, white weathering component reflects older gneiss package, which has been intruded and foliated with m-scale bodies of alkali feldspar granite (lith 2), features mm scale laminae, with mm to cm scale layer parallel leucosome, alternating with m scale bands of alkali feldspar granite.  Main lith is granitic component, minor lith represents rhythmically layered component. Seeing mesoscopic folds in same orientation as foliation.	main lithology	gneiss	orthogneiss	hornblende	20-50%	plagioclase	10-20%	biotite	20-50%	light grey to grey	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Cm-scale, gneissic layering of very quartz-rich, highly strained, recrystallized rock; protolith unclear; very recrystallized and qtz feldspar layers are interlayered with biotite rich layers. Very pyritic and potentially sillimanite bearing, but more likely chlorite. This component is also strongly magnetic, and likely features magnetite. Injected with in situ leucosome.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	20-50%	quartz	20-50%	plagioclase	10-20%	buff to pink	foliated	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Fine to medium grained.	FOL - Foliation	245	64	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2085-1	whole-rock lithogeochemistry	Mix of granitic and pegmatitic material. Pegmatite melt features kspar, probable albite, and quartz in a fine-grained biotite matrix. Not much biotite.	AL-23-2085-2	whole-rock lithogeochemistry	Rhythmically layered, grey component of gneiss in contact with pink, k spar granite component.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2086	07-07-2023 14:26:37.858	59.819422	-110.176762	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	380	-9999	-9999	-9999	-9999	Average 380 cps, all in all there is protomylonitic to mylonitic orthogneiss (Lith 1; moderately magnetic) being intruded by a younger, pink weathering granite.  Lenses/ rafts of schist stuff, down by shore ir grades into mylonite to ultramylonite, with feldspathic porphyroclasts wrapped up in dark grey material with felsic leucosomal mm to cm scale layering.  Sample AL-23-2086-3 is lens/raft of mafic schist with amphibolite composition. Mineralogy of granite gneiss is similar to previouw station. Rafts of amphibolite features an abundance of biotite, likely retrograding from hornblende., mixed with plag, quartz, minor muscovite (?) and/or pyrite/ other sulfides.	main lithology	mylonite	orthogneiss	biotite	10-20%	hornblende	20-50%	plagioclase	5-10%	dark to light grey	gneissic	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Very fine to cryptocrystalline; dark grey, alternating with felsic layers, layering is mm scale, ultramylonitic; extremely hard.	minor lithology	gneiss	alkali-feldspar granite	biotite	>50%	-9999	-9999	-9999	-9999	buff to pink	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Fine to medium grained, very hematized.	FOL - Foliation	225	87	Foliation intense	Increasingly mylonitic south towards shore.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2086-1	whole-rock lithogeochemistry	Granite gneiss, lith 2.	AL-23-2086-2	whole-rock lithogeochemistry	Mylonite verging on ultramylonite down by shore, orthogneiss Lith 1.	AL-23-2086-3	whole-rock lithogeochemistry	Lens/raft of mafic schist with amphibolite composition.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2087	07-07-2023 15:32:29.592	59.814865	-110.212130	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	4000	-9999	-9999	-9999	Measurements - 3400 cps, and 4000 cps,	main lithology	gneiss	granite	alkali-feldspar	>50%	quartz	10-20%	-9999	-9999	reddish pink, intensely hematized	gneissic	equigranular	phaneritic fine (0.5-1mm)	Fine to medium grained, locally pegmatitic, generally higher counts per second in these areas. Pegmatite is cross cutting the granite, and is extremely rich in biotite. Locally there are rafts of chlorite- biotite schist. M-scale quartz veins. Overall it is a mylonitized granite gneiss; sample 3 is down by the boat, represents white weathering mylonitized relict orthogneiss. Sample 4 is interlayered amphibolite (is this sillimanite bearing and the same as the chlorite - biotite rafts component?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	45	84	Foliation strong	Taken near amphibolite sample.	AXF - Axial fold plane	236	75	Foliation weak	79->250; hingeline of major fold, with high cps in core.	AXF - Axial fold plane	193	88	-9999	60->004; 2nd set of folds down by water; other set of folds from this location plunges 64-> 047; axial plane is 230/80.	AL-23-2087-1	whole-rock lithogeochemistry	Pegmatite, 4000 cps.	AL-23-2087-2	whole-rock lithogeochemistry	Background granite, up to 800 cps.	AL-23-2087-3	whole-rock lithogeochemistry	White weathering mylonitized relict orthogneiss.	AL-23-2087-4	whole-rock lithogeochemistry	Interlayered amphibolite, is this sillimanite bearing and the same as the chlorite-biotite raft component?	Alberta Geological Survey
AL-23-2088	07-07-2023 16:24:32.007	59.814244	-110.211461	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	1000	-9999	1700	-9999	-9999	-9999	Location of trench (1m wide by several meters in length) clearly blasted, exposing mylonitic to ultramylonitic granite gneiss. Anywhere in trench shows about 1000-1700 cps. Taking sample.	main lithology	gneiss	ultramylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	215	56	Foliation intense	Orientation of sample.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2088-1	oriented thin section	Oriented sample, features foliation and lineation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2089	09-07-2023 09:23:52.980	59.933444	-110.262017	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	420	-9999	2887	-9999	-9999	-9999	Pink weathering, alkali feldspar granite with in situ leucosome and quartz ribbons. Medium to coarse grained and locally pegmatitic. Appears to be intruding a more mafic gneissic package, and later folded with it. Calla's notebook: alkali-feldspar granite, hematized, local pegmatite and qtz veins, alternating coarse-grained and pegmatitic layers. Measurements - Scint avg background 287 - 420 cps, highs of 617 - 745 cps.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	-9999	-9999	-9999	pink weathering	foliated	-9999	phaneritic medium (1-5mm)	Highly hematized; between 287-428 cps background. Seeing lots of leucosome, and biotite schist interlayers (rare, local; which may represent melanosome or potential paleosome). North-trending folds.	minor lithology	gneiss	orthogneiss	biotite	>50%	feldspar	20-50%	quartz	10-20%	white	gneissic	-9999	-9999	Local, rare, may be getting its gneissic texture from injection of alkali feldspar granite.	FOL - Foliation	170	51	Foliation moderate	-9999	AXF - Axial fold plane	354	84	-9999	76->170.	-9999	-9999	-9999	-9999	-9999	AL-23-2089-1	whole-rock lithogeochemistry	K-spar granite.	AL-23-2089-2	whole-rock lithogeochemistry	Potential older gneissic package.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2090	09-07-2023 10:19:32.802	59.934273	-110.265281	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same lithology as station 89; appears increasingly gneissic moving to the north west, seeing increased amount of amphibolite pods and isoclinally folded biotite chlorite schist (Sillimanite?), often found wrapping leucosome. To the north, dextral offset of amphibolite schist along a vertical qtz vein oriented 130. Intermediate schist layers appear more psammopelitic and gritty.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	reddish buff to dark grey	foliated	porphyritic	phaneritic medium (1-5mm)	Fine to pegmatitic, various grain size phases. Increased amount of biotite; leucocratic melt patches feature pitted, tabular minerals which have completely weathered out (hbl? Tourmaline?).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	178	87	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2090-1	whole-rock lithogeochemistry; thin section	K-spar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2091	09-07-2023 11:03:27.705	59.935410	-110.266528	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz vein (m-scale) to the east (quartzite?) layer parallel pegmatite with alkali feldspar granite gneiss, pegmatite is also coming in axial planar to F2. Fold interference via F2 on F1, pegmatite interlayered within F1 folds with granite and amphibolite/schisty layers, with pegmatite coming in along axial planar to F2. Lots going on, sample 3 is granite gneiss and 4 is pegmatite.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	buff	gneissic	-9999	-9999	Potential layer of quartzite to the east; more likely a quartz vein but seems quite impure; (sample 1); Moving to the north begin to see biotite pegmatite selvage (broken leucosomal pegmatite suspended within potential amphibolites, which are featured within and folded with the granitic gneiss). Callas notes: Foliation 248.70; epidote veins layer parallel, and along contacts between mafic and felsic gneissic layers.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	221	80	-9999	-9999	AXF - Axial fold plane	175	83	-9999	76->338; F2, dominant, with F1 folds folded about its axis; associated S2 cleavage is 150/78. Weak, overprinting S-main.	AXF - Axial fold plane	70	88	-9999	Fold interference, this is the earlier set, F1, which are folded around structure type 2. F1 hingeline is: 74->234.	AL-23-2091-1	whole-rock lithogeochemistry	Quartz mixed with gneiss.	AL-23-2091-2	whole-rock lithogeochemistry	Amphibolite, contact with pegmatite.	AL-23-2091-3	whole-rock lithogeochemistry	Granite gneiss.	AL-23-2091-4	whole-rock lithogeochemistry	Pegmatite.	Alberta Geological Survey
AL-23-2092	09-07-2023 12:02:05.601	59.940876	-110.264215	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	1000	5	23.3	5	Foliated granite, with biotite rich matrix and k spar; regular kicks on spec uo to 1000cps, sporadic and within small m scale patches. Assay - 3.7 ppm U, 5% K, 23.3 ppm Th.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2092-1	whole-rock lithogeochemistry	Hot granite, 1121 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2093	09-07-2023 12:26:24.523	59.940364	-110.263102	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Biotite pegmatite selvage of alkali feldspar granite origin; 80-90 percent biotite possibly retrograding from hornblende, with mm to 5mm scale grains of kspar.  Bonny fault expressed as fault scarp, sharp contact between second lithology; the biotite rich main lith is graphitic, with a blueish grey sheen. Tough to distinguish from biotite.  Transition from main, biotite kspar rich main lith into 2m of kspar granite, into lithology 2 across the fault. Main lith is cataclastic and locally brecciated.  Locally more banded and layered, but a textbook gneiss. There is a definitive fabric but its loose, with lots of disorganization. Potentially mylonitic in some areas, with highly strained feldspathic material along foliation. layer parallel qtz leucosome in amphibolite patches, and layer parallel pegmatitic melt, albeit mostly rich in biotite matrix. ACROSS FAULT; 7 m wide zone of silicification, calling this lith two. Then back into biotite k spar graphite (main lith) cont lith 2.	main lithology	cataclastite	granite	biotite	>50%	alkali-feldspar	10-20%	graphite	10-20%	buff to greenish grey	schistose	porphyritic	-9999	The Bonny Fault is expressed as an extremely silicified m-scale fault scarp (see structures for more information); 7m zone; on the northeast, moving back into main lithology, abundant quartz stockwork and local quartz crackle breccia (sample 4).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	More gneissic on other side, seeing a more prominent foliation and more organization, abundant quartz stockwork oriented foliation parallel and 340/77 (oblique conjugate).	FOL - Foliation	353	87	Foliation moderate	Southwest side of fault, lith 1.	FT - Fault Brittle	155	70	-9999	Contact is the same orientation as the fault; pervasive conjugate fracture set oriented 265/85.	FOL - Foliation	4	86	Foliation strong	-9999	AL-23-2093-1	whole-rock lithogeochemistry	Hot kspar pegmatite selvage, up to 2800 cps, can be traced in strike length for 15-20 m, and is 1-2 m wide.  Several meters to the southwest of contact with lithology 2,  which is expressed by fault scarp (eastern Bonny Fault contact).	AL-23-2093-1B	whole-rock lithogeochemistry; thin section	Silicified fault rock.	AL-23-2093-3	whole-rock lithogeochemistry	Sample 3 is more of sample 1B a few meters northeast.	AL-23-2093-4	whole-rock lithogeochemistry	Brecciated and graphitic components of moving out of fault zone, quartz stockwork.	Alberta Geological Survey
AL-23-2094	09-07-2023 13:38:08.196	59.940290	-110.261920	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	15000	5.2	43.3	5.2	Biotite kspar graphite granite gneiss, with layers of amphibolite; pink and grey gneiss; 15000 cps beneath vegetation, took sample, only a 1m wide zone of intense radioactivity. Assay: #56 in scint, K: 5.2 %, U:329.8 ppm, Th: 43.3 ppm.	main lithology	gneiss	granite	biotite	>50%	alkali-feldspar	10-20%	graphite	10-20%	buff to grey	foliated	porphyritic	phaneritic fine (0.5-1mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	173	71	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2094-1	whole-rock lithogeochemistry; thin section	Hot kspar pegmatite beneath vegetation (15000 cps).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2095	09-07-2023 14:04:59.657	59.940227	-110.259425	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	338	-9999	12035	2.6	1189	2.6	Different weathering character, tannish cream, to greyish dusty brown; appears more sedimentary; mylonitic and displaying gneissic layering of fine grained, garnet, biotite and sillimanite bearing mm to cm scale schist with pelitic to psammopelitic quartzofeldspathic layers, with very coarse grained to pegmatite. Background cps is 338 to 467; high in pegmatite of up to 12035 cps (Assay #57, K: 2.6%, U: 239.2 ppm, Th: 1189 ppm); Most likely migmatite, with the paleosome (40-50%) comprised of pelitic to psammopelitic layers, with roughly 20-30% granitic to pegmatitic leucosome, and roughly 10-25% melanosome (bio sil schist).	main lithology	mylonite	paragneiss	garnet	10-20%	sillimanite	10-20%	-9999	-9999	tannish cream to dusty grey brown	gneissic	migmatitic	-9999	Compositional layering, of pelitic feldspathic layers with bands of garnets and sillimanite, the garnet intensely recrystallized and associated with leucosome, seeing felsic melt enveloping garnets; bands of smeared put garnets and sillimanite are cm scale, and continuous; 20m to east, within swamp crop, seeing much more paleosome, with lesser leucosome and melanosome; however, still seeing bands of pegmatitic leucosome; up to a m wide; pelitic to psammopelitic layers interlayered with quartzite; younger, coarser grained pegmatite cross cutting everything at 160; probably related to dominant folding; this gen of peg is massive. Can confirm layer of mylonite in between sediments and magnetic high to the west. Sediments become more happy, less mylonitized to the east.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	194	77	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2095-1	whole-rock lithogeochemistry; thin section	Paragneiss.	AL-23-2095-2	whole-rock lithogeochemistry; thin section	Hot pegmatite (12000 cps), may represent pegmatite leucosome.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2096	09-07-2023 16:34:54.137	59.946073	-110.266685	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	5.9	102.4	5.9	Orthogneiss, cream to dark grey/black, very magnetic and injected lit par lit by pink granite, which is further attenuated and sheared with the older package. Large amphibolite lenses and schlieren up to 3 metres long and half a meter wide. Large, porphyroclasts of feldspar wrapped up in mylonitic foliation, over 10cm in size.	main lithology	metatexite	orthogneiss	feldspar	20-50%	quartz	20-50%	biotite	20-50%	dark grey to white	protomylonitic	migmatitic	phaneritic fine (0.5-1mm)	Locally pegmatitic. Quite a bit going on here. Highly strained, well-layered white to buff weathering component is intruded by lit par lit injections of alkali-feldspar granite, which has been further strained and boudinaged. Local zones of intense shearing; late brittle faulting oriented with m-scale dextral offset. Older gneissic component is extremely magnetic, and is made up of mafic, cm scale layers of probably hornblende, magnetite, biotite, plagioclase, etc. alternating with more quartzofeldspathic layers and injections of k spar granite. Callas notes: K: 5.9%, U:14.0ppm, Th: 102.4ppm.	sheet	granitoid	alkali-feldspar granite	biotite	20-50%	alkali-feldspar	>50%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	205	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2096-1	whole-rock lithogeochemistry	Pegmatite.	AL-23-2096-2	whole-rock lithogeochemistry	Granite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2097	09-07-2023 17:12:46.016	59.945481	-110.262526	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	4.9	102.4	4.9	Younger k-spar granite injecting an older granite gneiss which alternates on the mm- to cm- scale from buff to white weathering, quartzofeldspathic layers to biotite rich, mafic layers, extremely magnetic; two orientations of foliation; one that the possible older component bears, and one that doesnt seem to affect the younger k spar (?) not sure; older foliation, which is associated with potentially older gneiss package, may reflect mesoscopic shear zones of granite gneiss which is highly strained and quartzofeldspathic, with gritty, non interlocking grains aligned parallel. Mini shear zone's foliation bends into main foliation on either side. Maybe the same granite, just more sheared/ gneissic in some areas. Assay - Th: 102.4ppm, U 14ppm; 4.9% K.	main lithology	metatexite	orthogneiss	feldspar	20-50%	quartz	20-50%	biotite	20-50%	dark grey to white	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Z-fold asymmetry given by folded quartz leucosome within amphibolite schlieren/lenses. Contradicts sinistral shearing within mini shear zone.	sheet	granitoid	alkali-feldspar granite	biotite	20-50%	alkali-feldspar	>50%	-9999	-9999	buff to tan	foliated	porphyritic	phaneritic fine (0.5-1mm)	Fine to coarse grained, locally pegmatitic.	FOL - Foliation	159	90	Foliation intense	Represents orientation of shearing, S-plane 159/90, c plane is 131/90. Sinistral sense of shear, qtz epidote veins coming in along roughly same orientation.	FOL - Foliation	255	89	Foliation moderate	Older foliation outside of shear zone, reflects dominant foliation of granite gneiss. This foliation bends into shear zone om either side.	-9999	-9999	-9999	-9999	-9999	AL-23-2097-1	whole-rock lithogeochemistry	Young, massive granite.	AL-23-2097-2	whole-rock lithogeochemistry; thin section	More granite.	AL-23-2097-3	whole-rock lithogeochemistry; thin section	Silicified orthogneiss.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2098	10-07-2023 08:59:37.554	59.934737	-110.258697	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	200	-9999	720	5.4	38.9	5.4	Alkaki feldspar granite, foliated but not gneissic, its intensely hematized. Measurements - cps: between 200-350 cps, high of 720.  Assay: 5.4% K, 15.5 ppm U, 38.9 ppm Th.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	5-10%	biotite	1-5%	reddish buff	foliated	porphyritic	phaneritic fine (0.5-1mm)	Foliation given by quartz leucosome wrapped by biotite melanosome; locally migmatitic, locally massive; 20% neosome, of 10-15% being leucosome and the remainder melanosome. paleosome is pink, alkali feldspar granite, contains amphibolite lenses.	minor lithology	schist	amphibolite	biotite	>50%	hornblende	10-20%	plagioclase	10-20%	dark grey	schistose	porphyritic	cryptocrystalline (<0.1mm)	Contains fragmented k spar grains suspended in the matrix.	FOL - Foliation	133	81	Foliation weak	Given by foliated neosome.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2098-1	whole-rock lithogeochemistry	Amphibolite component.	AL-23-2098-2	whole-rock lithogeochemistry; thin section	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2099	10-07-2023 10:03:25.480	59.938070	-110.273590	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	3.1	42.3	3.1	Purple mineral (cm-scale) caught my eye, appears to be lepidolite (purple mica) in a biotite schist. Tiny swampside outcrop; K: 3.1% U: 2.3 ppm U; Th:42.3 ppm; assay 59; not fluorite, its LEPIDOLITE; and appears to be mostly an alteration mineral on the weathering surface. Potential sillimanite.	main lithology	schist	intermediate schist	fluorite	1-5%	sillimanite	1-5%	garnet	<1%	greyish light buff	schistose	porphyritic	phaneritic very fine (0.1-0.5mm)	Lepidolite in a biotite qtz matrix, looks pelitic in origin. Garnet is questionable, there is a solid amount of kspar grains wrapped by sillimanite in a biotite quartz matrix spotted with opaques and silvery, cubic sulfides. There is also minor muscovite, 5-10%, and potential chalcopyrite. Slightly magnetic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	163	81	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2099-1	whole-rock lithogeochemistry; thin section	Intermediate schist, lepidolite present?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2100	10-07-2023 11:01:36.091	59.942182	-110.275978	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Sheared, cataclastic to locally mylonitic TBC gneiss, with extensive quartz stockwork; p and g gneiss, locally disorganized and faulted, fresh surface shows quartz epidote leucosome, (mm-scale) foliation parallel, alternating with greenish, cryptocrystalline biotite chlorite hornblende matrix with potential sillimanite.  Matrix is basically aphanitic, cant see crystal boundaries but gut is telling me there is hornblende and biotite breaking down to chlorite, alternating with qtz ep leucosome and granitic kspar and quartz.	main lithology	mylonite	diatexite	chlorite	10-20%	epidote	5-10%	alkali-feldspar	10-20%	dark grey to pink	gneissic	migmatitic	cryptocrystalline (<0.1mm)	Very silicified. Pink represents paleosome, while dark grey layers appear to represent biotite-rich enveloping melanosome; paleosome unrecognizable.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	253	86	Foliation moderate	-9999	FT - Fault Brittle	305	86	-9999	Orientation of brittle fracture and major conjugate orientation of quartz stockwork, coming in along joints. Other orientation is foliation parallel. Offset observed but movement direction not super clear. Seeing locally dextral offset of qtz leucosome.	-9999	-9999	-9999	-9999	-9999	AL-23-2100-1	whole-rock lithogeochemistry	Silicified granite/mylonitic migmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2101	10-07-2023 11:44:04.773	59.943949	-110.271910	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Within apparent TBC, gneissic and protomylonitic kspar granite with biotite sillimanite schist mafic layers.	main lithology	gneiss	protomylonite	alkali-feldspar	20-50%	chlorite	1-5%	alkali-feldspar	20-50%	brownish buff	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Fine grained matrix with cm-scale porphyroclasts of kspar.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	265	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2101-1	whole-rock lithogeochemistry	Protomylonitic kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2102	10-07-2023 11:50:08.071	59.944330	-110.272337	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	2510	7.8	275	7.8	Increasingly mylonitic to the west, reduction of porphyroclast grain size, way more exposure here then 101. Feldspar porphyroclasts of kspar in the mm scale to half cm scale, wrapped by mylonitic, intermediate to mafic cryptocrystalline matrix. Layer parallel quartz leucosome and epidote staining along foliation plane. Intersection of faults, one oriented 070/69; conjugate is 240/69.	main lithology	gneiss	protomylonite	biotite	20-50%	alkali-feldspar	10-20%	quartz	20-50%	-9999	-9999	porphyritic	-9999	Calla's notebook: Assay 61 (K:4.6%, U: 16.3 ppm, Th: 207.1 ppm); Assay #62 (2510 cps) K: 7.8%, U: 14.1 ppm, Th: 275.0 ppm; at intersection of fault.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	203	69	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2102-1	whole-rock lithogeochemistry	Hot (2300 cps) protomylonitic kspar granite.	AL-23-2102-2	whole-rock lithogeochemistry; thin section	Protomylonitic kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2103	10-07-2023 13:08:38.177	59.947543	-110.271702	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	980	5.8	102.8	5.8	Down by the water, lakeshore outcrop; lithology goes through transitional contact mear waters edge; from granitic mylonitic gneiss into potential mylonitized quartzite and pelitic layers (lith 2) with mixed biotite granitic gneiss content interlayered; this may also be a mini shear zone, with ribboned feldspars and qtz; seems to reflect similar lithology. Most likely just an increase in strain moving northeast.	main lithology	mylonite	mylonite	biotite	20-50%	alkali-feldspar	20-50%	chlorite	20-50%	reddish pink to buff	gneissic	porphyritic	aphanitic (<0.01mm)	No crystal boundaries, suspended k spar grains oriented along foliation planes, 70% biotitic, retrograding from hornblende to chlorite, matrix with probable saussurite (recrystallized plagioclase). 2 meters from water, see transitional; protomylonite to full mylonite, porphyroclasts of kspar up to one quarter of a cm. Assay results: 980 cps; K: 5.8% U: 2.2 ppm; Th: 102.8 ppm; in mini shear zone, C plane is oriented foliation parallel, S plane is 165/81; dextral CS; shear zone/sediments carry K:2.3% U: 3.8ppm, Th: 36.6 ppm, less potassium. Probable transition, albeit sheared, into metasedimentary gneiss.	minor lithology	mylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	153	65	-9999	-9999	FT - Fault Brittle	243	62	-9999	-9999	FT - Fault Brittle	315	80	-9999	-9999	AL-23-2103-1	whole-rock lithogeochemistry	Granitic component.	AL-23-2103-2	whole-rock lithogeochemistry	Biotite rich, highly-strained component.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2104	10-07-2023 14:27:22.922	59.944586	-110.280416	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	2.7	23	2.7	Beautiful, mylonitic, migmatized gneiss; over 60% melt, abundant mafic schlieren, and xenolith lenses up to 3 m long and 1-2 m wide, which are elliptical in shape, and pinching out into tails on either end; dextral shear sense based on orientation and shape of xenoliths. Two sets of folds, one foliation parallel and one refolding this.  Xenoliths are folded with gneissic paleosome and leucosome, and are cut by foliation parallel leucosome.  Additionally, there are massive pods of foliated kspar granite, 2 m long and 1 m wide, which are also cut by qtz leucosome and are wrapped by the very biotite rich mylonitic foliation.  Assay #66: K=6.5%, U=1.5 ppm, Th = 5.5 ppm.  Assay #67: K=0.8%, U=1.0 ppm, Th = 5.8 ppm.  Assay #68: K = 1.0 %, U = 2.7 ppm, Th = 21.9 ppm.  Assay #69: K = 4.8%, U=4.4 ppm, Th = 35.1 ppm.  Assay #70: K=3.6%, U=1.5 ppm, Th=5.1 ppm.  Assay #71: K=2.7%, U=3.3 ppm, Th=23.0 ppm; dextral asymmetric Z folds.	main lithology	mylonite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	buff to cream, with dark grey to black layering	gneissic	migmatitic	-9999	Full on mylonitized migmatite; paleosome reflected by mafic rich, mylonitic gneissic matrix; injected by m-scale sheets of alkali-feldspar granite, which are further sheared and attenuated into the mylonitic fabric; large, m-scale lens of this, with tails pinching out. Abundant mafic schlieren with quartz leucosomal layering. Discordant foliations with respect to dominant fabric. Paleosome is a recrystallized, mafic paste interlayered with injections of granite, which feature mafic schlieren suspended within, and biotite-rich melanosome interlayered and enveloping the paleosome.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	226	63	Foliation intense	Anastomosing, dominant mylonitic fabric.	AXF - Axial fold plane	190	78	-9999	Plunge= 70-195; 83-190, 011/90; 87-185, 180/90.	AXF - Axial fold plane	336	90	-9999	Dominant younger set, plunge 85->160; 144->86, 342/89.	AL-23-2104-1	whole-rock lithogeochemistry	Gneissic component (paleosome injected with leucosome, or is it leucosome and melanosome?).	AL-23-2104-2	whole-rock lithogeochemistry; thin section	Amphibolite component (schlieren).	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2105	10-07-2023 15:57:39.607	59.937698	-110.281581	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	871	3.8	82.9	3.8	No notes captured.	main lithology	gneiss	protomylonite	biotite	>50%	plagioclase	20-50%	alkali-feldspar	20-50%	alternating greenish grey and pink (fresh)	gneissic	porphyritic	cryptocrystalline (<0.1mm)	K spar porphyroclasts up to 1cm in length, suspended in biotite, plagioclase, chlorite, probable hornblende and saussurite matrix, green and waxy, indistinguishable crystal boundaries, protomylonite verging on mylonite; 3.8 K, 5.5 ppm U, 82.9 ppm Th, high of 871 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	222	80	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2105-1	whole-rock lithogeochemistry	Protomylonite verging on mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2106	11-07-2023 08:37:22.086	59.819402	-110.181171	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	190	600	-9999	-9999	-9999	Quartz leucosome coming in vertically along 110 trend (see lithology notes for more applicable station notes). Anastomosing foliation, bending around vertical. K-spars suspended in matrix of hornblende, saussurite, chlorite, potential cordierite. Sample 3: rusty boulder. Measurements - Scint avg background 90 cps, highs of 600 cps.	main lithology	gneiss	granite	alkali-feldspar	>50%	biotite	10-20%	quartz	20-50%	dark grey to buff	gneissic	equigranular-xenomorphic	phaneritic medium (1-5mm)	Biotite rich layers probably contain hornblende and plagioclase, both of which have begun to break down and retrogress. Waxy texture, cm-scale gneissic banding. Sample AL-23-2106-3 is rusty boulder.	minor lithology	schist	amphibolite	biotite	20-50%	hornblende	20-50%	plagioclase	10-20%	black, reflective	schistose	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Not as phyllonitic as observed in other places.	FOL - Foliation	74	86	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2106-1	whole-rock lithogeochemistry	Granite gneiss.	AL-23-2106-2	whole-rock lithogeochemistry	Amphibolite phyllonite.	AL-23-2106-3	whole-rock lithogeochemistry	Rusty boulder - not an insitu sample.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2107	11-07-2023 09:10:34.378	59.817292	-110.185190	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	210	550	-9999	-9999	-9999	Pink weathering, foliated and locally massive alkali feldspar granite, intruding an older gneissic component which is folded with lenses of amphibolite. Main lith is alkali granite, 2nd lith is gneissic component; background is 210 cps, high of 550 cps. To be clear, the younger granite is dominant and pervasive, and seems to be interlayered biotite-rich schist (is this melanosome or amphibolite, shredded?) orthogneiss almost completely phased out,	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	10-20%	biotite	10-20%	buff	massive	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Classic, massive, weakly foliated k spar granite.	minor lithology	gneiss	orthogneiss	quartz	20-50%	plagioclase	10-20%	biotite	10-20%	cream	gneissic	equigranular-xenomorphic	cryptocrystalline (<0.1mm)	Extremely fine grained, not seeing the aluminous minerals; grain boundaries indistinct, probable hornblende retrograding to biotite, along with potential muscovite. Appears as if these bands of quartzofeldspathic (possible quartzitic) material are interla	FOL1 - Foliation gen1	155	90	Foliation strong	This fabric is most prominent in the gneiss, general structural trend; however, foliation is very folded and amastomosing.	AXF - Axial fold plane	70	84	-9999	74->254, younger, overprinting set; S2 associated cleavage axial planar.	AXF - Axial fold plane	240	73	-9999	87->010; this is refolded by F2, taken from sinistral limb of F2 folds.	AL-23-2107-1	whole-rock lithogeochemistry	Massive, weakly foliated k spar granite.	AL-23-2107-2	whole-rock lithogeochemistry	Orthogneiss component with injections of granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2108	11-07-2023 09:56:40.163	59.817268	-110.191088	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	250	430	-9999	-9999	-9999	Alkali feldspar granite (lith 2) intruding and being foliated with an older, locally gneissic rock which makes up a small amount of outcrop.  The older rock features a very mafic matrix, extremely fine grained and with hornblende retrograding to biotite, but more hornblende in this one. Appears to bear a classic granite composition, however, its more intermediate due to the immense amount of mafic; >60% fine grained mafic matrix, not seeing as many flakes as before, definitely some hornblende.  Half cm scale layering of kspar and qtz and biotite, hornblende and plagioclase.  Mafic layers may contain sulfides, and there is waxy, broken down saussurite looking mineral which was probably plagioclase that makes up 10-20 percent. qtz is 20-50%; av cps: 250, high of 430.	main lithology	gneiss	granodiorite	alkali-feldspar	10-20%	plagioclase	20-50%	quartz	20-50%	tan to light grey	gneissic	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Locally verging on gneissic.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	10-20%	-9999	-9999	buff	foliated	equigranular-hypidiomorphic	phaneritic fine (0.5-1mm)	Locally massive and pegmatitic, and interlayered with small lenses of amphibolite, which is extremely biotite rich and retrograding to chlorite, with possible sillimanite, also bearing tiny, silvery gold reflective sulphides, not apparently magnetic.	FOL - Foliation	195	90	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2108-1	whole-rock lithogeochemistry	Represents lith 2, k spar granite and amphibolite.	AL-23-2108-2	whole-rock lithogeochemistry	older, more intermediate foliated granite verging on gneissic.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2109	11-07-2023 10:45:09.610	59.818913	-110.199492	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	120	250	330	-9999	-9999	-9999	Verging on mylonitic, well foliated alkali feldspar granite down by the shore; 10 meters in, start seeing layering of alkali feldspar granite with white weathering amphibolite with black phenocrysts up to half a cm in size. Measurements - Scint background 250 cps, max of 330 cps; Scint avg 120 cps in lith 2 (amphibolite).	main lithology	mylonite	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	greyish buff	foliated	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Intensely foliated and recrystallized k spar granite, bands are mm-scale of kspar quartz alternating with biotite and possible relict hornblende. Appears mylonitic.	minor lithology	schist	amphibolite	hornblende	>50%	biotite	20-50%	plagioclase	10-20%	cream	schistose	porphyritic	phaneritic medium (1-5mm)	Coarsest amphibolite observed, it's probably gabbroic in origin, cream grey weathering in comparison to dark grey black interlayers of phyllonite amphibolite. Half cm black phenocrysts are magnetic (magnetite?) and locally make up to 10% of the rock. Blac	FOL - Foliation	246	60	Foliation strong	Locally not as intense.	AXF - Axial fold plane	118	90	-9999	80->110; hinge.	-9999	-9999	-9999	-9999	-9999	AL-23-2109-1	whole-rock lithogeochemistry	Mylonitic granite.	AL-23-2109-2	whole-rock lithogeochemistry; thin section	Med-grained magnetic amphibolite. Gabbroic, magnetite?	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2110	11-07-2023 11:25:10.943	59.813753	-110.209974	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	380	900	-9999	-9999	-9999	Alkali feldspar hornblende granite with amphibolite interlayers and lenses. Measurements - background cps: 380; high of 900. Geochem analysis should help us understand the magnetic change compared to last station.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	hornblende	10-20%	quartz	10-20%	reddish pink	foliated	porphyritic	phaneritic coarse (5-10mm)	Medium to coarse grained with hornblende porphyry, which are clearly breaking down to biotite.	minor lithology	schist	amphibolite	biotite	-9999	plagioclase	-9999	-9999	-9999	dark grey to black	foliated	-9999	-9999	No notes captured.	FOL - Foliation	115	90	Foliation weak	Locally massive kspar granite, anastomosing around vertical and refolded, folds observed axial planar to S-main.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2110-1	whole-rock lithogeochemistry; thin section	Alkali feldspar hornblende granite.	AL-23-2110-2	whole-rock lithogeochemistry	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2111	11-07-2023 12:47:58.250	59.812957	-110.214045	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Migmatite, with sillimanite biotite and possible relict garnet bearing compositional bands up to 2cm wide, amphibolite interlayers, layer parallel alkali feldspar granite and layer parallel biotite pegmatite selvage.  Two sets of folds, ribboned feldspars and quartz, potential layers of quartzite could also be leucosome.	main lithology	diatexite	diatexite	sillimanite	1-5%	biotite	>50%	alkali-feldspar	20-50%	buff, cream, and grey	gneissic	migmatitic	-9999	Paleosome is likely a gneissic granite, grey coloured and broken down into leucosome enveloped and suspended within biotite rich melanosome. Keep in mind Godfrey has quartzite/high-grade meta-sediments mapped close to this. Mesoscopic M-folds (W depending on plunge direction) are prominent.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	7	83	-9999	65->7; hinge of earlier F1 set.	AXF - Axial fold plane	95	84	-9999	84->090; late set of folds, refolding early set; hook style.	AL-23-2111-1	whole-rock lithogeochemistry; thin section	Main lithology, mix of migmatitic components.	AL-23-2111-2	whole-rock lithogeochemistry	Amphibolite schlieren.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2112	11-07-2023 13:28:51.929	59.813090	-110.221625	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Folded, gneissic granite; pink alkali feldspar granite interlayered with potential quartzite and gritty pelitic layers. Definite compositional layering mixed with the younger granite. Compositional banding of pink granite and grey biotite and potentially sillimanite bearing amphibolite, with gritty appearance, suggests its a gneiss. Banding over 10cm scale, these things are folded doubly.	main lithology	gneiss	metatexite	hornblende	20-50%	plagioclase	10-20%	quartz	20-50%	buff	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Looks more like diorite, gneissic paleosome; toeing the line between metatexite and diatexite; older, dioritic component makes up ~30% of the outcrop. Mafic schlieren and injections of kspar granite (more dominant and closely related with schlieren) are interlayered and doubly folded. Potential dextral shear bands.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	220	73	Foliation strong	-9999	AXF - Axial fold plane	213	80	-9999	72->350; hinge of F2 folds, creating type 3 via F2 on F1.	AXF - Axial fold plane	216	76	-9999	79->036; hinge of isoclinal, foliation S-main parallel F1 folds.	AL-23-2112-1	whole-rock lithogeochemistry; thin section	Migmatite paleosome, diorite gneiss?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2113	11-07-2023 14:20:22.845	59.814492	-110.247618	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	900	-9999	2500	-9999	-9999	-9999	Foliated kspar granite and amphibolite, interlayered. Anomalous hot zone of 900-1500 cps traced along strike for 15 m, 1-2 m wide. Sample from here. Locally pegmatitic, with chunks of kspar up to a few cms in size are suspended in biotite chlorite matrix.  Another hot anomalous zone up to 2500 cps a few meters across strike to the northwest, well hematized all around, blue quartz and/or potential hematite.	main lithology	gneiss	alkali-feldspar granite	quartz	10-20%	alkali-feldspar	>50%	biotite	5-10%	buff	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	No notes captured.	minor lithology	schist	amphibolite	biotite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	50	90	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2113-1	whole-rock lithogeochemistry	Hot (over 2000 cps) foliated kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2114	11-07-2023 15:10:06.995	59.816801	-110.267323	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	White weathering white and grey gneiss; garnet bearing.	main lithology	metatexite	paragneiss	garnet	1-5%	sillimanite	1-5%	plagioclase	20-50%	cream to grey	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Ribboned qtz and feldspar with garnets and possible sillimanite, garnets up to half a cm in size and also micro, within fine graimed matrix; in situ quartzofeldspathic leucosome, potentially mylonitized quartzite. Pelitic matrix; garnets also appear smeared and are clearly retrograding to flaky biotite; more intact garnets are within leucosome component; plag porphryoclasts in qtz and biotite rich matrix with bluish sheen, possible molybdenite and definite sulphides; definitely migmatized. Highly-strained; are these primary garnets or melt garnets? Is there cordierite in the melt?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	322	82	Foliation intense	-9999	AXF - Axial fold plane	145	64	-9999	90->258; hinge.	-9999	-9999	-9999	-9999	-9999	AL-23-2114-1	whole-rock lithogeochemistry; thin section	White and grey gneiss, garnet bearing (Min ID; melt/metamorphic relations).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2115	11-07-2023 15:43:49.453	59.815859	-110.269147	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	More of the mylonitic, migmatized, white weathering paragneiss with garnets up to a few cms in size, either equant or strung out in foliation. Garnets, in pelitic quartzofeldspathic and biotite rich matrix. Possible molybdenite (irredescent bluish purple silvery reflective mica enveloping garnets), possibly sillimanite and cordierite(?), probable sulphides and muscovite.	main lithology	mylonite	paragneiss	garnet	1-5%	feldspar	10-20%	quartz	10-20%	cream to light grey	gneissic	porphyritic	phaneritic very fine (0.1-0.5mm)	Garnet porphyry, and clear compositional layering, with layer parallel quartz leucosome; garnet in sandy, pelitic to psammopelitic bands as well as leucosome; cm-scale tabular, elongate mineral weathering out; andalusite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	15	83	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2115-1	whole-rock lithogeochemistry; thin section	Chips of garnet bearing pelite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2116	11-07-2023 16:35:34.161	59.809975	-110.268487	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	150	-9999	210	-9999	-9999	-9999	-9999	-9999	-9999	Back into TBC alkali feldspar granite and amphibolite. Higher strain, mm-cm scale layering and mylonitic fabric.	main lithology	gneiss	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	50	83	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2116-1	whole-rock lithogeochemistry	Alkali feldspar granite.	AL-23-2116-2	whole-rock lithogeochemistry	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2117	13-07-2023 08:49:51.443	59.819297	-110.215230	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	200	450	-9999	-9999	-9999	Contact between older, gneissic dark grey weathering rock and pink weathering, intruding and being foliated with it. Alternatively, the dark grey, biotite, hornblende, plag +/- qtz -bearing rock, given a gneissic texture by layer parallel leucosome, may represent amphibolite gabbro, potentially associated with the intrusive granite.	main lithology	gneiss	unsubdivided gneiss	biotite	20-50%	feldspar	10-20%	quartz	10-20%	dark grey	gneissic	migmatitic	phaneritic very fine (0.1-0.5mm)	Layer parallel leucosome, biotite rich quartzofeldspathic matrix with xenoblastic equigranular grain boundaries.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	210	84	Foliation strong	Mirrors contact with alkali feldspar granite; however, foliation is weak in the granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2118	13-07-2023 09:31:17.887	59.820150	-110.221466	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	170	-9999	350	-9999	-9999	-9999	Buff weathering kspar granite gneiss (m-scale, sharp boundaries) injecting/intruding m-scale unit of layered biotite rich amphibolite, dark grey to black weathering, with sulphides. Measurements - lith 1, granite gneiss: 350 cps average, amphibolite: 170 cps, pegmatite: 220 cps.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	20-50%	biotite	20-50%	cordierite	1-5%	dark grey	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Black phenocrysts of glossy, conchoidal nature with bluish tint; cordierite? Looks like obsidian. Up to half a cm in size and foliated, within mafic component of granite gneiss; layer parallel leucosomal biotite albite rich pegmatite, with biotites on the cm scale and plagioclase up to several cm in length, found within the grey unit and also as melt patches within the granite. I believe this is called in-source leucosome, sourcing from the granite and melting into the older, grey package. Granite is locally massive.	sheet	schist	amphibolite	biotite	>50%	feldspar	10-20%	quartz	10-20%	dark grey	schistose	porphyritic	phaneritic very fine (0.1-0.5mm)	Fine-grained matrix with hornblende porphyry which locally resemble pyroxene; lots of biotite, retrograding from the black blocky mineral. Potential cordierite? Sulphide bearing 12 m layer of amphibolite at this station. Could this be melanosome? These la	FOL - Foliation	10	90	Foliation strong	Anastomosing. Measurement taken at shoreline.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2118-1	whole-rock lithogeochemistry	K-spar granite gneiss; gneissic layering.	AL-23-2118-2	whole-rock lithogeochemistry	Lith 2, amphibolite and pegmatite melt; is this amphibolite or an older orthogneiss?	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2119	13-07-2023 10:16:02.663	59.820545	-110.223555	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	280	-9999	-9999	-9999	-9999	Buff weathering granite gneiss with half m scale lenses of amphibolite; appears mylonitic and recrystallized, with mesocopic, m-scale S folds of the granite gneiss and the amphibolite, with pegmatite coming in axial planar. Sinistral shearing along the axial plane of these folds (prominent). There are patches which may resemble the original paleosome, which has been heavily injected by alkali-feldspar granite.	main lithology	mylonite	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	buff	gneissic	migmatitic	phaneritic medium (1-5mm)	Mm scale layering of mafic and felsic gneissic components; feldspar and qtz slightly ribboned; locally massive; well foliated overall. Sample taken from more massive kspar granite, medium to coarse grained, verging on mylonite.	enclave	mylonite	amphibolite	biotite	>50%	amphibole	10-20%	plagioclase	10-20%	-9999	schistose	porphyritic	phaneritic fine (0.5-1mm)	K-feldspar and quartz grains in chloritic, biotite and plagioclase rich matrix; biotite plag, and hornblende coarse grained, 5-10 mm in scale in fine grained pelitic matrix; gritty and features layer parallel pegmatitic melt of biotite and albite.	FOL - Foliation	25	85	Foliation intense	-9999	AXF - Axial fold plane	53	85	Foliation weak	80->244; hinge line; aplite dike coming in along axial fold plane; m-scale S fold of amphibolite lens, refolding S-main, which lens bears; lens also features mm scale compositional layering.	-9999	-9999	-9999	-9999	-9999	AL-23-2119-1	whole-rock lithogeochemistry	Main lithology, sample taken from more massive kspar granite, verging on mylonite.	AL-23-2119-2	whole-rock lithogeochemistry; thin section	Highly strained amphibolite enclave.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2120	13-07-2023 10:57:42.329	59.821203	-110.224924	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same rocks, paleosome is increasingly mylonitic to the northwest and constitutes grey weathering, quartzofeldspathic and biotite, hbl, plag rock injected with alkali-feldspar granite. Difficult to say how much of the grey weathering component is paleosome vs melanosome; seeing more disorganization of foliation and increased amount of in situ fine grained leucosome probably derived from kspar granite.  Migmatitic here.	main lithology	metatexite	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	paleosome	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	grey	-9999	-9999	-9999	Grey, recrystallized, quartzofeldspathic + biotite, hbl -bearing rock may represent source rock. Given striped texture by injections of alkali-feldspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2120-1	whole-rock lithogeochemistry; thin section	Orthogneiss component; or is this mafic melanosome enveloping felsic melt? If true, it is diamictite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2121	13-07-2023 11:19:03.900	59.823128	-110.227433	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	400	7000	-9999	-9999	-9999	Highly strained; granitic gneiss with m scale amphibolite lens, with layer parallel alkali feldspar granite leucosome; background of 400 cps; local anomalous 2-3 m zone of up to 7000 cps, open northeast along strike; traced for 15-20 m downstrike. Pegmatite is kspar phenocrysts in very fine grained biotite matrix with abundant very fine grained qtz and feldspar; sulphides as well.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	reddish buff	gneissic	migmatitic	phaneritic medium (1-5mm)	Locally pegmatitic and massive; interlayered with grey weathering amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	335	85	-9999	-9999	FOL - Foliation	70	77	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2121-1	whole-rock lithogeochemistry; thin section	Biotite pegmatite, up to 7000 cps; foliation of zone is anastomosing, 077/77.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2122	13-07-2023 12:08:05.519	59.825312	-110.222297	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	360	-9999	-9999	-9999	-9999	Interlayered amphibolite and kspar granite; compositional bands of mafic seems to be of the same composition of the S folded amphibolite enclaves; verging on gneissic, locally well foliated and also more massive in areas.  Layer parallel in situ leucosome of kspar and quartz, in addition to quartz epidote veins which are both locally layer parallel and coming in along fractures.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	20-50%	biotite	20-50%	quartz	10-20%	buff	gneissic	migmatitic	phaneritic fine (0.5-1mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	13	85	Foliation strong	Fabric is refolded by gentle sw-ne trending folds, to the east the foliation bends clockwise; abundant S folds given by folded enclaves of amphibolite, which seems to make up at least compositionally the mafic gneissic bands that alternate with the (?).	FT - Fault Brittle	280	90	-9999	250/90 is conjugate set; sigma 1 oriented 010 and 090 vertical; amphibolite enclave showing grabben structure, down faulted along vertical fractures.	-9999	-9999	-9999	-9999	-9999	AL-23-2122-1	whole-rock lithogeochemistry	K-spar granite gneiss with mafic interlayers, verging on gneissic.	AL-23-2122-2	whole-rock lithogeochemistry	Amphibolite enclave.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2123	13-07-2023 13:56:34.406	59.825501	-110.232813	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	250	2000	-9999	-9999	-9999	Older white and dark grey. Measurements - Scint average 250 cps, high of 2000 cps within younger k spar granite.	main lithology	gneiss	orthogneiss	biotite	>50%	amphibole	10-20%	quartz	10-20%	dark greyish buff	gneissic	equigranular	phaneritic fine (0.5-1mm)	Fine to medium grained, grey and white granite; white layers are quartzofeldspathic with probable plagioclase; mafic layers are biotite rich and likely sulphide bearing. Potential muscovite along foliation plane; mm to 5 mm scale layering; clearly intruded by younger granite which is massive.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2123-1	whole-rock lithogeochemistry	Orthogneiss, white weathering and mylonitic.	AL-23-2123-2	whole-rock lithogeochemistry	Intruding, buff-weathering granite component (kspar granite?) highs of 2000 cps.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2124	13-07-2023 14:44:27.539	59.823093	-110.238042	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	260	450	-9999	-9999	-9999	Lichenite with granite gneiss (diatexite); weakly foliated kspar granite with porphyry of obsidian looking mineral with blueish tinge and conchoidal fracture; cordierite(?) half cm in size; certainly diatexite if considering felsic, pink component as the leucosome and the biotite schist as the melanosome.	main lithology	granitoid	diatexite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	buff	foliated	porphyritic	phaneritic medium (1-5mm)	Background cps: 250 cps; fine to medium grained k spar granite with amphibolite enclaves on the half m scale; biotite is extremely fine grained and makes up cm scale masses, leaving a mottled, weathered appearance as if the amphibolite is interlayered; the migmatitic and intruding nature of the kspar granite into the amphibolite makes it appear as if they are interlayered; local pegmatite of megacrystic grain size, sheets of biotite up to 10cm in width and length, with kspars and pure quartz almost as large; sample 3 is this super coarse grained pegmatite. Amphibolite has a mixed quartzofeldspathic composition, could this be remnants of a paleosome, mostly converted to melanosome?	enclave	schist	amphibolite	biotite	>50%	plagioclase	20-50%	quartz	10-20%	dark grey	schistose	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Cryptocrystalline; extremely fine grained matrix of biotite, highly altered and broken down plagioclase along with pelitic quartz and feldpspar; gritty and not interlocking.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2124-1	whole-rock lithogeochemistry	Main lithology, granite gneiss diatexite.	AL-23-2124-2	whole-rock lithogeochemistry; thin section	Amphibolite/magnetic orthogneiss?	AL-23-2124-3	whole-rock lithogeochemistry	Extremely coarse-grained pegmatite melt, books of biotite 10cm in width/length, 1cm thick and grains of quartz and feldspar just as large.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2125	13-07-2023 15:51:41.685	59.819668	-110.240009	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	450	4500	-9999	-9999	-9999	Margin of major thorium high; getting up to 4500 cps in local pegmatitic melt; av cps: 450.	main lithology	gneiss	alkali-feldspar granite	biotite	>50%	alkali-feldspar	10-20%	quartz	5-10%	light greyish buff	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	6	87	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2125-1	whole-rock lithogeochemistry; thin section	K-spar granite gneiss, up to 4500 cps.	AL-23-2125-2	whole-rock lithogeochemistry	Amphibolite component.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2126	14-07-2023 09:15:43.094	59.813165	-110.236415	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	10000	-9999	-9999	-9999	Pegmatite dike, trenched; within amphibolite schist with layer parallel leucosome, in situ and derived from large, intruding bodies of potential Colin Lake granite; which is dominated by quartz (>50%), feldspar (20-50), and 5-10 % biotite retrograding to chlorite; weakly, magnetic in places. AL-23-2126-3 is this lith; AL-2126-4 comes from western pegmatite trench (10m long and similar counts per second). Oriented parallel to foliation; eastern trench is perpendicular to it (sample 1). Also seeing small bodies of Uranium City granite (kspar granite).	main lithology	gneiss	orthogneiss	biotite	>50%	feldspar	20-50%	quartz	10-20%	grey and white	schistose	migmatitic	phaneritic very fine (0.1-0.5mm)	Layer parallel leucosome injections with plagioclase up to a couple cm in size are well foliated and lend the rock a gneissic appearance; crack it open and its a pelitic looking biotite schist with some hornblende and sulfides; very magnetic; leucosome is folded. Likely that it is the older orthogneiss package, experiencing abundant partial melting.	dike	granitoid	pegmatite dike	biotite	>50%	alkali-feldspar	20-50%	quartz	5-10%	dark grey weathering	massive	-9999	pegmatitic	Very magnetic; potential pyrite/pyrrhotite.	FOL - Foliation	163	75	Foliation moderate	Orientation of foliation parallel pegmatite dike.	AXF - Axial fold plane	195	78	Foliation strong	70->019; hinge line; associated axial planar cleavage.	IGC - Contacts	215	77	-9999	Contact between quartzofeldspathic granite, foliation parallel. Granite layer is 2 m wide.	AL-23-2126-1	whole-rock lithogeochemistry; thin section	Pegmatite dike, 10000 cps and within trench, perpendicular to foliation.	AL-23-2126-2	whole-rock lithogeochemistry; thin section	Main lith, orthogneiss.	AL-23-2126-3	whole-rock lithogeochemistry	Colin Lake granite?	AL-23-2126-4	whole-rock lithogeochemistry	Pegmatite from western side of trench, oriented parallel to foliation.	Alberta Geological Survey
AL-23-2127	14-07-2023 10:42:34.047	59.808863	-110.233493	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Lichenite; appears mafic; dirty, fine grained matrix with lots of smoky quartz, mixed with waxy highly altered plagioclase, with a decent amount of biotite and some hornblende. Potential microgarnets, and definite silvery copper coloured sulfide (pyrite?); sediment stuff at station point, moving to more southern outcrops, we see kspar granite coming in along noted foliation; on weathered surface main lith appears gneissic, with greenish grey bands up to 2cm wide alternating with the dark grey bands; upon breaking it open it is impossible to distinguish the mineralogical differences; tough to say if its truly gneissic; could be a schist.	main lithology	gneiss	orthogneiss	quartz	20-50%	plagioclase	20-50%	biotite	10-20%	dark grey	schistose	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Bearing some hornblende and sulfides.	sheet	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	10-20%	hornblende	5-10%	buff	foliated	equigranular-xenomorphic	phaneritic medium (1-5mm)	Hornblende beginning to retrograde to biotite, with inclusions of probable pyrite/sulfides.	FOL - Foliation	355	87	Foliation moderate	Parallels contact with kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2127-1	whole-rock lithogeochemistry	Orthogneiss, intermediate rock.	AL-23-2127-2	whole-rock lithogeochemistry	Uranium City equivalent, kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2128	14-07-2023 11:36:41.449	59.810551	-110.238485	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	2500	-9999	-9999	-9999	Foliated to gneissic Uranium City/ kspar granite, with biotite rich amphibolite schist interlayers; locally massive;  potential orthogneiss at sample 2 site; sample 3 is mylonite granite gneiss oriented, sample 4 is hot peg, 2500cps at sample site 3. Samples 3 & 4 verging on mylonitic; orthogneiss with kspar granite injections and leucosome, with pegmatitic melt rich in biotite (recorded as Litho2).	main lithology	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	buff	gneissic	migmatitic	phaneritic medium (1-5mm)	Well foliated, verging on gneissic; more banded to the west.	minor lithology	gneiss	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	215	86	Foliation moderate	-9999	FOL - Foliation	112	90	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2128-1	whole-rock lithogeochemistry; thin section	Hot, weakly foliated kspar granite (2500 cps).	AL-23-2128-2	whole-rock lithogeochemistry	Potential mylonitic orthogneiss.  Sample collected aprx. 47 m SSE from station (coords. 59.81015164; -110.23822716).	AL-23-2128-3	whole-rock lithogeochemistry	Diatexite mylonite granite gneiss (over 60% melt (schist + granite) oriented. Sample collected aprx. 67 m SW from station (coords. 59.81010843; -110.23927366).	AL-23-2128-4	whole-rock lithogeochemistry	Hot pegmatite (~2500 cps). Sample collected aprx. 67 m SW from station (coords. 59.81010843; -110.23927366).	Alberta Geological Survey
AL-23-2129	14-07-2023 13:11:39.506	59.814964	-110.248057	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pink and black, typical TBC kspar granite and interlayered bioitite schist of previously amphibolite. Two phases of pegmatite, one foliation parallel and one axial planar to major folding.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	buff and dark grey	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Fine to medium.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	230	70	Foliation moderate	244/75 up the hill to the west.	AXF - Axial fold plane	356	90	-9999	61->365; hinge.	-9999	-9999	-9999	-9999	-9999	AL-23-2129-1	whole-rock lithogeochemistry	K-spar granite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2130	14-07-2023 14:12:32.454	59.815832	-110.249885	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Continued from structure note: the mafic xenoliths are probably getting sheared and melted with the kspar granite, forming layering of biotite schist and quartzofeldspathic leucosome; orientation of mafic xenolith parallels fold axis (S2) and dike contact; epidote coming in along S2 foliation.	main lithology	diatexite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Diatexitic, paleosome can be picked up as white and grey weathering orthogneiss, magnetic, more apparent moving to the west. Abundant mafic schlieren suspended in biotite rich pegmatitic melt.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	241	66	-9999	-9999	FOL2 - Foliation gen2	230	81	Foliation weak	Axial planar to folding of amphibolite and k spar granite; orientation of kspar dike fine to med grained, cross-cutting earlier apparently gneissic layering of amphibolite and the kspar granite; mafic xenoliths appear like schlieren.	AXF - Axial fold plane	15	84	Foliation weak	65->020; hinge. Gentle, folds which affects the S-main fabric, bending it clockwise.	AL-23-2130-1	whole-rock lithogeochemistry; thin section	Pegmatite biotite melt; kspar suspended in biotite rich matrix.	AL-23-2130-2	whole-rock lithogeochemistry	Main lith, diatexite - paleosome orthogneiss?	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2131	14-07-2023 15:11:11.568	59.812900	-110.255659	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	K-feldspar granite with m-scale amphibolite lenses, associated with biotite pegmatite selvage of the intruding kspar granite and leucogranitic, layer parallel melt with prominent quartz epidote veining and alteration along foliation. K-feldspar granite is interlayered with biotite schist, potentially aluminum silicate bearing. Foliated kspar granite with amphibolite, locally pegmatitic and massive.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	biotite	>50%	quartz	10-20%	buff and black	foliated	equigranular-xenomorphic	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2131-1	whole-rock lithogeochemistry	K-spar granite.	AL-23-2131-2	whole-rock lithogeochemistry	Biotite rich amphibolite cut by pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2132	14-07-2023 15:22:30.596	59.813579	-110.255374	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alkali feldspar granite folded with amphibolite lenses and interlayers; amphibolite is very green locally, and is both parallel with the granite about an east trending axis, and also intruded and cut by the granite.  Granite is foliated along fold limbs but massive within fold hinge, suggesting that the granite may be nosing its way into fold hinges during progressive deformation; probably why we see layer parallel in situ leucosome of kspar with the amphibolite.	main lithology	diatexite	diatexite	alkali-feldspar	>50%	quartz	10-20%	biotite	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	100	72	Foliation strong	Axial fold plane.	FOL1 - Foliation gen1	195	78	-9999	Sinistral limb of massive, open fold. Dextral limb is fol 2; fold hinge is 79->040; earlier folds foliation parallel refolded by this structure.	FOL2 - Foliation gen2	15	81	-9999	Dextral fold limb.	AL-23-2132-1	whole-rock lithogeochemistry	Diatexite kspar granite, well foliated and verging on gneissic, given by loose banding of kspar quartz alternating with biotite schist.	AL-23-2132-2	whole-rock lithogeochemistry	Green amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2133	14-07-2023 16:30:06.940	59.812126	-110.263673	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Well foliated kspar granite; patches of amphibolite, but dominantly kspar granite.  Epidote and qtz leucosome layer parallel.	main lithology	granitoid	alkali-feldspar granite	alkali-feldspar	-9999	biotite	-9999	quartz	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FT - Fault Brittle	100	88	-9999	Mineral stretching lineation? Oriented 050->100.	FOL - Foliation	185	78	Foliation strong	-9999	AL-23-2133-1	whole-rock lithogeochemistry	K-spar granite, well foliated.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2134	15-07-2023 08:43:15.034	59.947241	-110.286626	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Biotite granite gneiss; Uranium City granite with small, lenses of amphibolite, often interlayered with sharp lithologic boundaries; featuring rare enclaves of amphibolite on the m-scale, wrapped by near-mylonitic foliation. Augen feldspars (<2cm) and near ribbon quartz grains bring out the highly-strained nature of these rocks. The sharp interlayering suggests the younger biotite granite may be injecting an older, mafic rock.	main lithology	gneiss	alkali-feldspar granite	alkali-feldspar	>50%	biotite	20-50%	quartz	10-20%	buff	gneissic	equigranular-xenomorphic	phaneritic medium (1-5mm)	Seeing black conchoidal qtz with blueish tinge; same stuff i said looked like obsidian. Porphyrytic, if you count this; some hornblende on its way down through biotite. The mineral is most likely black quartz.	main lithology	mylonite	alkali-feldspar granite	biotite	>50%	alkali-feldspar	20-50%	quartz	5-10%	dark grey with buff interlayers	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Recrystallized.	FOL1 - Foliation gen1	183	80	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2134-1	whole-rock lithogeochemistry	K-spar biotite granite gneiss (Uranium City equivalent).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2182	21-07-2023 16:18:16.211	59.756003	-110.104390	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	White and grey well foliated granodiorite intruded by quartzofeldspathic leucogranitic pegmatite; m-scale layering. Could this be the same as the sediments we saw at Spider Lake, rather than granodiorite? Need to compare samples.	main lithology	gneiss	granodiorite	quartz	20-50%	plagioclase	20-50%	biotite	20-50%	light grey	foliated	migmatitic	phaneritic fine (0.5-1mm)	Fine to medium grained.	leucosome	granitoid	pegmatite sill	feldspar	>50%	biotite	5-10%	quartz	5-10%	white	massive	equigranular-idiomorphic	pegmatitic	Melt patches.	FOL - Foliation	164	74	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2182-1	whole-rock lithogeochemistry; oriented thin section	Granodiorite, diorite component.	AL-23-2182-2	whole-rock lithogeochemistry	Pegmatite of albite, probable k spar, and biotite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2183	21-07-2023 17:06:11.659	59.755929	-110.105559	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	3000	7.6	28.4	7.6	Incredible exposure of mylonitic Colin Lake and granodiorite unit from previous station, migmatitic mm scale layering of the two components, in contact with potential mylonitic metasediments with compositional layering of pelitic and psammopelitic appearing components. This unit has cryptic layering, with abundant in layer parallel white leucosome, with melanosome layers, and grey quartzofeldspathic layers. Probably diatexite. Measurements - 3000 cps in Colin Lake pegmatite with yellow staining; Assay #76 - U: 153.1ppm; Th: 28.4ppm; K: 7.6%.	main lithology	mylonite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Interlayered and intruded by Colin leucogranitic pegmatite with yellow uranium staining hitting 3000 cps.	raft	mylonite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	145	85	Foliation intense	-9999	AXF - Axial fold plane	95	90	-9999	80->084; hinge of later set of folds, especially noticable in the sediments.	AXF - Axial fold plane	10	90	-9999	87->190 hinge of early set of folds; pervasive and ptygmatic.	AL-23-2183-1	whole-rock lithogeochemistry	Potential paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1061	28-06-2023 11:57:15.081	59.879776	-111.014573	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Significant shearing in outcrop. Recrystallized rock. Lots of magnetite. Chlorite and epidote replacement. Traces of retrogressed garnet. Small lenses of granite pegmatite that post dates the shearing.	main lithology	mylonite	mesomylonite	chlorite	<1%	garnet	<1%	magnetite	<1%	-9999	-9999	-9999	phaneritic medium (1-5mm)	No notes captured.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	Granite pegmatite sheet.	FOL - Foliation	28	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1061-1	whole-rock lithogeochemistry	Recrystallized mylonite, lots of magnetite, chlorite and epidote replacement.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1062	28-06-2023 12:59:02.897	59.881339	-111.007934	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Amphibolite and biotite schist - 10% mafic sheets.  Orthogneiss is pink, coarse grained.	main lithology	gneiss	orthogneiss	biotite	5-10%	graphite	-9999	-9999	-9999	pink	-9999	-9999	-9999	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	5	79	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1062-1	whole-rock lithogeochemistry	Granite - trace chlorite.	LL-23-1062-2	whole-rock lithogeochemistry; thin section	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1063	28-06-2023 13:28:53.699	59.884406	-111.011103	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.7	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Spotted migmatite near the shore. Porphyroclasts are seen up the hill. MS 0.7. This is a very mixed outcrop with lots of folds.	main lithology	mylonite	mylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1064	28-06-2023 13:40:30.999	59.884522	-111.012297	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Just up the hill from last outcrop. Garnet is 5-10% of the rock (up to 4cm) with crenulated sillimanite. There are lots of melt zones here, locally migmatitic. Lots of quartz veining locally. High scintillometer readings. 2 channel samples were collected.	main lithology	gneiss	paragneiss	garnet	1-5%	graphite	<1%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1064-1	whole-rock lithogeochemistry; thin section	Garnet sillimanite paragneiss.	LL-23-1064-2	whole-rock lithogeochemistry; thin section	Garnet sillimanite paragneiss, radiometric anomalies.	LL-23-1064-C1	whole-rock lithogeochemistry	Paragneiss channel saw sample from elevated cps location.	LL-23-1064-C2	whole-rock lithogeochemistry	Paragneiss channel saw sample from elevated cps location.	Alberta Geological Survey
LL-23-1065	28-06-2023 14:48:07.665	59.896768	-111.003258	Internal GPS	Alex MacNeil	Russell Hartlaub	0.3	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	Near Cu-Au MAR record. Ribboned quartz in a medium grained recrystallized quartzofeldspathic rock. Lots of quartz veining at N end of outcrop. Huge outcrop. Measurements - MS 0.3 up to 2.	main lithology	mylonite	mesomylonite	chlorite	1-5%	biotite	1-5%	-9999	-9999	vibrant pink	-9999	-9999	phaneritic coarse (5-10mm)	Uniform granite. Qtrz veins and foliation deflected from main trend.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	325	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1065-1	whole-rock lithogeochemistry	Mylonite quartzofeldspathic rock.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1066	28-06-2023 15:30:10.371	59.896984	-111.006200	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Good outcrop. Cross-cutting quartz veins. Local episode associated with veins. Paragneiss at the shore with spotted migmatite up the hill. Heterogeneous layering.	main lithology	gneiss	paragneiss	garnet	5-10%	biotite	10-20%	chlorite	1-5%	-9999	-9999	-9999	-9999	Looks like sillimanite in spots. isoclinal folds in some places.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	VN - Vein	170	75	-9999	Qtz 2 cm thick sub-parallel.	FOL - Foliation	196	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1066-1	whole-rock lithogeochemistry; thin section	Garnet paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1067	29-06-2023 09:24:36.083	59.789748	-111.061679	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Halo used. Traverse on west side of Leland Lake. Huge amount of amphibolite here (30% of outcrop). The orthogneiss (MS 0.15) locally has patches of a brown weathering mineral that could be hypersthene.	main lithology	mafic rocks	orthogneiss	biotite	10-20%	hornblende	5-10%	chlorite	<1%	-9999	-9999	-9999	phaneritic coarse (5-10mm)	No notes captured.	minor lithology	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL1 - Foliation gen1	200	78	-9999	-9999	FT - Fault Brittle	155	70	-9999	Sinistral with qtz.	LINF - Lineation fold	15	55	-9999	-9999	LL-23-1067-1	whole-rock lithogeochemistry; thin section	Mafic, coarse crystalline amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1068	29-06-2023 09:53:44.280	59.789705	-111.064008	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	8	-9999	-9999	-9999	-9999	-9999	-9999	Continuation of unit from 1067. Some magnetism. MS up to 8.	main lithology	mafic rocks	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	206	62	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2053	30-06-2023 10:00:40.463	59.733339	-111.211694	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Three variations of grain size/ phases of this Slave batholith. The pegmatite appears to be a product of in-situ melting of the med-grained phase, while the third phase reflects a fine-grained aplite apparently cuts the other phases. Locally Well foliated, with biotite/chlorite porphyry flattened along foliation.	main lithology	granitoid	granitoid	quartz	20-50%	plagioclase	20-50%	alkali-feldspar	5-10%	white to cream	foliated	-9999	pegmatitic	Weakly- to moderately foliated, and locally massive. Probably muscovite, plag extremely sericitized -> definite fluid alteration. Interlayered with more fine grained sills of similar composition with what appears to be sausserite porphyroblasts of plag+/-epidote, chlorite, and biotite parentage. General increase in size of pegmatite grains. Roughly 50% pegmatite late melt material to 50% coarse grained material.	sill	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	foliated	porphyritic	phaneritic fine (0.5-1mm)	Represents the fine-grained granite phase, which makes up 20-30% of outcrop.	-9999	178	88	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2053-1	whole-rock lithogeochemistry	Fine-grained granite dike.	LL-23-2053-2	whole-rock lithogeochemistry	Med-grained granite component of outcrop.	LL-23-2053-3	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2054	30-06-2023 11:37:05.893	59.732764	-111.209023	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Spectral OH endmember site, with highly altered and smoothed out slope surface (south facing) showing relationship between fine, medium, and pegmatite phases of previous station. Here we started seeing spots of extremely retrogressed and xenoblastic garnet, or at least with the garnet colouring. Med grained is main lith, dominant, and together with the pegmatitic variety, have been the dominant rock type all day. Pegmatite appears to be melting in situ out of the med-grained phase, which are both cut by the fine-grained, aplite dikes.	main lithology	granitoid	granitoid	-9999	-9999	-9999	-9999	-9999	-9999	light greyish brown, to cream to buff pink	foliated	equigranular	phaneritic medium (1-5mm)	Including the pegmatite phase with this lith, roughly 60% med grained, 20-30% peg of similar composition, with rubbed out potential garnet. The pegmatite cuts the med grained, and the fine grained sills/ dikes cut both med and peg. Sample of med, and peg.	minor lithology	granitoid	sill	-9999	-9999	-9999	-9999	-9999	-9999	-9999	foliated	porphyritic	-9999	No notes captured.	IGC - Contacts	180	90	-9999	Pegmatite dike cross cutting main lith.	VN - Vein	170	90	-9999	Coarse pegmatite	FOL - Foliation	18	90	-9999	In dike. Overprints dike, picked up by porphyry. Is dominant foliation.	LL-23-2054-1	whole-rock lithogeochemistry; thin section	Med-grained granite with potential garnet.	LL-23-2054-2	whole-rock lithogeochemistry	Fine-grained granite.	LL-23-2054-3	whole-rock lithogeochemistry	Pegmatite, with purple quartz.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2135	15-07-2023 08:57:59.415	59.947747	-110.285450	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Protomylonite to mylonite; granite gneiss with quartz epidote leucosome cutting the foliation and giving dextral shear sense; ribboned qtz and feldspar; interlayered with biotite schist; kspar and/or plagioclase; potential sulphides. Featuring rare enclaves of amphibolite on the m-scale, wrapped by near-mylonitic foliation. Augen feldspars (<2cm) and near ribbon quartz grains bring out the highly-strained nature of these rocks. The sharp interlayering suggests the younger biotite granite may be injecting an older, mafic rock.	main lithology	gneiss	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	179	67	Foliation intense	Mylonitic foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2135-1	whole-rock lithogeochemistry	Granite gneiss mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2136	15-07-2023 09:12:14.685	59.948777	-110.282407	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Not mylonitic, sheared than previous outcrop	main lithology	gneiss	alkali-feldspar granite	plagioclase	10-20%	hornblende	20-50%	alkali-feldspar	>50%	buff	gneissic	porphyritic	phaneritic medium (1-5mm)	Fine to medium gneissic hornblende kspar granite with low quartz; plag porphyroclasts foliated, verging on mylonitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	188	78	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2136-1	whole-rock lithogeochemistry	Main lithology, gneissic hornblende kspar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2137	15-07-2023 09:42:27.085	59.948040	-110.288007	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Highly strained biotite granite gneiss; striae 90->130.	main lithology	gneiss	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	198	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2138	15-07-2023 10:01:50.154	59.942355	-110.297044	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Sheared, migmatitic kspar granite injecting older gneissic rock with mafic, recrystallized, dirty pelitic appearing matrix (not seeing aluminum minerals); young granite is being attenuated and sheared; abundant S folds, rare, localized Z-folds.	main lithology	metatexite	mesomylonite	hornblende	20-50%	quartz	10-20%	feldspar	5-10%	dark grey	gneissic	equigranular-xenomorphic	aphanitic (<0.01mm)	No notes captured.	minor lithology	intermediate schist	para-amphibolite	hornblende	20-50%	quartz	10-20%	feldspar	10-20%	dark grey	gneissic	equigranular-xenomorphic	aphanitic (<0.01mm)	Extremely fine grained matrix with slaty cleavage.	FOL - Foliation	190	72	Foliation intense	-9999	AXF - Axial fold plane	358	88	-9999	70->010; hinge of fold, parallel to S-main.	-9999	-9999	-9999	-9999	-9999	AL-23-2138-1	whole-rock lithogeochemistry	Migmatitic k spar granite.	AL-23-2138-2	whole-rock lithogeochemistry	Dirty pelitic rock which is gneissic and appears to be intruded and sheared with kspar granite; which is the dominant rock and contains amphibolite lenses which are interlayered as well.	AL-23-2138-3	whole-rock lithogeochemistry	Pegmatitic melt.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2139	15-07-2023 10:36:40.185	59.942608	-110.297522	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Beautiful exposure of chloritic, white and light grey gneiss in contact with kspar granite gneiss; mylonitic; main lith is extremely quartz rich, variably schistose to gneissic; in both cases appears to have a gritty, qtz rich matrix; transitional contact (grad) from quartzitic rock into massive to foliated kspar granite; contact parallels foliation; injections of the kspar granite in the quartzite is layer parallel, in situ; abundant layer parallel quartz and epidote leucosome.	main lithology	mylonite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	white to light grey	gneissic	-9999	-9999	Quartzite being injected by biotite granite, then metamorphosed and sheared lightly.	sheet	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	buff	gneissic	-9999	-9999	No notes captured.	FOL - Foliation	188	65	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2139-1	whole-rock lithogeochemistry; thin section	Schisty component of quartzite with lots of white clay/sericite and waxy plagioclase altered.	AL-23-2139-2	whole-rock lithogeochemistry; thin section	Quartzitic, gneissic component with ribboned mins.	AL-23-2139-3	whole-rock lithogeochemistry	Amphibolite interlayers.	AL-23-2139-4	whole-rock lithogeochemistry	Massive to foliated kspar granite.	Alberta Geological Survey
AL-23-2140	15-07-2023 11:46:09.952	59.886338	-110.308248	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	K-feldspar granite gneiss; mylonitic, with hornblende kspar layering; large enclaves of coarse grained amphibolite gabbro with hornblende and plag stringers multiple cm in length; enveloped in chlorite epidote vein which shows earlier foliation, being refolded and sheared by S main; cleavage refraction observed.	main lithology	granitoid	mesomylonite	alkali-feldspar	20-50%	hornblende	20-50%	quartz	10-20%	buff	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Fine to very fine, intensely hematized kspar gneiss with hornblende layers (magnetic) beginning to retrograde to feldspar. Up to cm sized plagioclase porphyroclasts (augen feldspar); high strain, ribbon qtz and feldspar.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	215	79	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2140-1	whole-rock lithogeochemistry; thin section	Mylonitic granite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2141	15-07-2023 12:19:46.201	59.885911	-110.307220	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Abundant mylonitic xenoliths of gabbro, bodies 0.5 m to 20m wide, wrapped in aphanitic, pink and grey, extremely recrystallized (mafic paste) meso-mylonite to ultra-mylonite; xenoliths are very coarse grained, hornblende biotite plagioclase low quartz; xenoliths of gabbroic amphibolite on the m- scale are wrapped by this intensely recrystallized mylonite; layer parallel leucosome; large xenoliths of amphibolite gabbro up to the m scale are wrapped by mylonitic foliation and forming tails.	main lithology	metatexite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	migmatitic	equigranular-xenomorphic	phaneritic coarse (5-10mm)	Xenoliths of gabbro are more dominant than the mafic, mylonitic matrix (lith 2) that they are suspended within. The mylonite comprises injections of pink leucogranite (alkali feldspar granite), amidst a mafic, pasty matrix (intensely recrystallized), with bodies of mylonitized gabbro suspended in the mylonitic fabric, in addition to schlieren and interlayers of amphibolite ranging from fine- to- coarse-grained.	xenolith	gabbroid	gabbro	biotite	>50%	hornblende	20-50%	plagioclase	10-20%	white and black	migmatitic	equigranular-hypidiomorphic	phaneritic coarse (5-10mm)	No notes captured.	FOL - Foliation	210	72	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2141-1	whole-rock lithogeochemistry; thin section	Gabbro injected by granite.	AL-23-2141-2	whole-rock lithogeochemistry; thin section	Mylonitic matrix.	AL-23-2141-3	whole-rock lithogeochemistry	Gabbro enclave.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2142	15-07-2023 13:48:54.656	59.884980	-110.306993	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mylonitized migmatite with m-scale sheared bodies of amphibolite gabbro with aphanitic, green porphyry (local). Gabbro is intruded and sheared with kspar granite and in situ layer parallel leucosome of pegmatite, quartz and epidote veins. Gabbro has been variably recrystallized, where the rock appears as a mylonitic orthogneiss it is probably grounded down gabbro, with kspar layer parallel leucosome. Local clasts of very coarse grained epidote with chilled margins, enveloped by lower strain gabbro within the high strain gabbro kspar mylonite.	main lithology	metatexite	mesomylonite	alkali-feldspar	20-50%	hornblende	>50%	plagioclase	20-50%	greenish dark grey and white	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Seeing abundance of xenoliths decrease; that is, the mylonitic matrix becomes more dominant moving east; and the gabbro becomes less interlayered and are more clearly present as schlieren and xenoliths, similar to the western stations covering this unit. Whereas in the center, the gabbro schlieren have been ground into the mylonite, interlayered with the injections of young pink granite.	xenolith	gabbroid	gabbro	biotite	20-50%	hornblende	20-50%	plagioclase	10-20%	white and black	migmatitic	equigranular-hypidiomorphic	phaneritic coarse (5-10mm)	No notes captured.	FOL - Foliation	210	72	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2142-1	whole-rock lithogeochemistry	Green aphanitic vein hosted mineral, associated with leucosome injection and foliated; this is most likely mafic schlieren.	AL-23-2142-2	whole-rock lithogeochemistry	Mylonite gabbro.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2143	15-07-2023 14:42:06.182	59.883825	-110.302569	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mylonitized gabbro alternating with potassium feldspar granite; similar to previous station but increased amount of kspar layering; biotite rich.	main lithology	metatexite	mesomylonite	alkali-feldspar	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	xenolith	gabbroid	gabbro	biotite	20-50%	hornblende	20-50%	plagioclase	10-20%	white and black	migmatitic	equigranular-hypidiomorphic	phaneritic coarse (5-10mm)	No notes captured.	FOL - Foliation	208	80	-9999	168/76 is orientation of relict foliation within amphibolite gabbro xenolith, discordant to dominant foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2143-1	whole-rock lithogeochemistry	Black green fine grained xenolith.	AL-23-2143-2	whole-rock lithogeochemistry	Host rock mylonite.	AL-23-2143-3	whole-rock lithogeochemistry; thin section	Gabbro enclave.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2144	15-07-2023 15:29:09.721	59.882103	-110.301242	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Cataclastic rock, gneissic; kspar alternating with aphanitic mafic layers; extremely recrystallized.  Pink eggshell, but underneath, a dark paste; moving west, there are large, triangular shaped, very angular amphibolite clasts caught up within the mylonitic granite.	main lithology	gneiss	cataclasite	alkali-feldspar	20-50%	hornblende	>50%	plagioclase	-9999	buff	gneissic	equigranular-xenomorphic	aphanitic (<0.01mm)	Brecciated biotite-hornblende granite gneiss; decreasing in strain to the east.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	198	66	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2144-1	whole-rock lithogeochemistry; thin section	Gneissic cataclastic rock.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2145	15-07-2023 16:10:06.269	59.885509	-110.309300	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same lithology as station directly up strike. stopped for oriented sample.	main lithology	granitoid	mesomylonite	alkali-feldspar	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2145-1	oriented thin section	Gneissic cataclastic rock, oriented sample.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2146	15-07-2023 17:07:53.204	59.916453	-110.291395	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartzite type rock with chlorite matrix, looks like what we saw earlier today on west side of lake. Interlayers of mafic, biotite schist up to 10 cm in size.	main lithology	mylonite	mesomylonite	alkali-feldspar	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Extremely quartz rich, darker colouration on fresh surface, pink eggshell on weathered.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	201	86	Foliation intense	Straie to 67.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2146-1	whole-rock lithogeochemistry; thin section	Quartzite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2147	15-07-2023 17:25:24.207	59.916435	-110.290065	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Out of quartzite, into mylonitic granite with chloritic, extremely fine grained biotite matrix and kspar porphyry.	main lithology	mylonite	protomylonite	alkali-feldspar	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	188	85	Foliation intense	Slaty cleavage, protomylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2147-1	whole-rock lithogeochemistry; thin section	Main lithology, protomylonitic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2148	16-07-2023 08:58:32.881	59.856784	-110.295371	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	400	2500	-9999	-9999	-9999	Grey and white orthogneiss; younger leucogranite layer parallel with older, grey component of dioitic to tonalitic composition; leucosome is turning into porphyroclasts, protomylonitic.	main lithology	gneiss	protomylonite	quartz	>50%	biotite	20-50%	plagioclase	20-50%	light to dark grey	gneissic	porphyritic	phaneritic medium (1-5mm)	Fine to medium grained; proto-mylonitic with quartzofeldspathic porphyroclasts wrapped by quartz, plagioclase, and biotite hornblende; compositional layering of extremely fine grained biotite, retrograding from hornblende and very altered and recrystallized plagioclase interlayered with more qtz and kspar rich layers. Appears to have gritty dirty matrix, likely pelitic, with layer parallel quartz feldspar melt; possible cordierite.	leucosome	granitoid	leucogranite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	190	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2148-1	oriented thin section	Protomylonitic orthogneiss.	AL-23-2148-2	whole-rock lithogeochemistry	Hot (2500 cps) leucogranite; melt layer.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2149	16-07-2023 09:32:40.699	59.855975	-110.294669	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large m-scale mesoscopic folds; verging on mylonitic (high strain, ribboned qtz feldspar) orthogneiss of similar composition as previous station but much more hornblende and biotite and less quartz rich. Intruded by kspar granite and folded with it, interlayered but dominantly mafic component here.	main lithology	mylonite	orthogneiss	hornblende	20-50%	biotite	20-50%	plagioclase	20-50%	buff to dark grey	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Abundant Z-fold asymmetry; grey and white orthogneiss injected by kspar granite, which is locally pegmatitic, layer parallel, and also axial planar to main fold set.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	205	80	-9999	89->021; hinge line; axial plane is parallel to S2 cleavage, which is very weak.	FOL1 - Foliation gen1	198	85	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2149-1	whole-rock lithogeochemistry; thin section	Protomylonitic orthogneiss, with kspar injection.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2150	16-07-2023 10:07:33.115	59.855758	-110.293044	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz and plag rich orthogneiss, with extremely fine grained biotite and hornblende; hornblende coming down to chlorite.	main lithology	metatexite	orthogneiss	quartz	20-50%	hornblende	20-50%	plagioclase	20-50%	cream to grey	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Fine to medium, with abundant layer parallel pegmatite melt, with plag crystals up to 10 cm mylonitic orthogneiss is highly strained.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2150-1	oriented thin section	Oriented orthogneiss 230/90, 55->230.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2151	16-07-2023 10:30:26.254	59.855278	-110.290524	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Into gneissic, ultramylonite of Uranium City granite with xenoliths of amphibolite, heavily mafic content; although there is a significant amount of hematized kspar component.	main lithology	gneiss	ultramylonite	quartz	>50%	hornblende	20-50%	alkali-feldspar	20-50%	buff	gneissic	equigranular-xenomorphic	cryptocrystalline (<0.1mm)	Mafic paste interlayered with kspar; significant amount of plagioclase; hornblende altering to biotite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Folation	185	89	Foliation intense	Anastomosing, wavering around vertical.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2151-1	whole-rock lithogeochemistry; thin section	Ultramylonitic granite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2152	16-07-2023 10:50:58.324	59.855109	-110.287955	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	White to buff weathering, mylonitized orthogneiss injected by kspar granite; intensely strained, mm- to cm-scale layering of orthogneiss, pink granite, and biotite schist (melanosome?).	main lithology	metatexite	orthogneiss	quartz	20-50%	plagioclase	20-50%	biotite	20-50%	cream to buff	gneissic	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Gneissic layering of quartz and plagioclase which are almost indistinguishable from each other; alternating with retrograde biotite (some hornblende); white and black on fresh surface.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	3	90	Foliation intense	Very recrystallized; mylonitic to ultramylonitic; mm scale layering of ribboned feldspars and qtz, alternating with biotite schist. Locally intruded by k spar granite, and by large chunks of qtz; local isoclinal folds parallel with foliation (F1).	AXF - Axial fold plane	265	90	-9999	78->245; hinge line F2.	-9999	-9999	-9999	-9999	-9999	AL-23-2152-1	whole-rock lithogeochemistry; thin section	Weathered and fresh surface, protomylonitic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2153	16-07-2023 11:22:16.981	59.855066	-110.287098	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Absolute chaos; intensely migmatized; impossible to break down into normal migmatite components; overall, the gneissic foliation is 130/90, with large xenoliths/potentially schlieren of amphibolite gabbro, which are foliated intensely but completely discordant to the dominant fabric.	main lithology	gneiss	diatexite	quartz	20-50%	feldspar	20-50%	biotite	20-50%	buff to grey, hematized	gneissic	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Fine to medium, orthogneiss (white and grey) similar to where we saw it earlier on traverse.	unknown	mafic rocks	amphibolite	hornblende	20-50%	plagioclase	20-50%	biotite	20-50%	dark grey	foliated	migmatitic	phaneritic medium (1-5mm)	Fine to medium, gabbro amphibolite, strong biotite foliation; hornblende dominant and retrograding to biotite.	FOL1 - Foliation gen1	140	84	Foliation intense	F1 isoclines oriented 177/88, S-main parallel.	FOL2 - Foliation gen2	55	90	-9999	Avergage orientation of relict foliation shown by mafic xenoliths, which have layer parallel qtz leucosome.	AXF - Axial fold plane	277	88	-9999	075->277; hinge, dominant fold style.	AL-23-2153-1	whole-rock lithogeochemistry	Amphibolite schlieren with quartz leucosome.	AL-23-2153-2	whole-rock lithogeochemistry	Migmatitic orthogneiss.	AL-23-2153-3	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2154	16-07-2023 12:04:09.614	59.854317	-110.282343	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Approaching magnetic high.	main lithology	gneiss	metatexite	hornblende	20-50%	biotite	20-50%	quartz	10-20%	buff to light grey	gneissic	migmatitic	phaneritic very fine (0.1-0.5mm)	Gritty, waxy intensely recrystallized, with biotite plus hornblende and plagioclase alternating (mm scale bands) with quartz and feldspar layers; interlayered with foliated kspar granite, orthogneiss may represent original paleosome; kspar amd biotite rich schisty layers may represent leucosome (coming from large body of kspar granite plus partial melting of gneiss) and melanosome.	leucosome	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	10-20%	biotite	5-10%	buff	foliated	equigranular-xenomorphic	phaneritic fine (0.5-1mm)	Fine to medium grained, biotite altering from hornblende.	AXF - Axial fold plane	285	90	-9999	Tight to open folds, cant read hinge.	FOL - Foliation	252	72	Foliation strong	Anastomosing and folded, a bit all over the place.	-9999	-9999	-9999	-9999	-9999	AL-23-2154-1	whole-rock lithogeochemistry	Main lithology, migmatitic orthogneiss.	AL-23-2154-2	whole-rock lithogeochemistry	K-spar granite leucosome.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2155	16-07-2023 13:48:28.332	59.858362	-110.280377	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Protomylonitic to mylonitic, ribbon feldspars; orthogneiss interlayered with k spar granite; mylonitic; with compositional layering; sinistral rotation of porphyroclasts; on the cusp of diatexite.	main lithology	mylonite	diatexite	biotite	>50%	magnetite	1-5%	plagioclase	20-50%	buff to cream	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Mafic component extremely magnetic; potential magnetite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	165	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2155-1	whole-rock lithogeochemistry	Mylonitic orthogneiss.	AL-23-2155-2	whole-rock lithogeochemistry	Coarser grained biotite dominated layer, very magnetic.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2156	16-07-2023 14:18:35.187	59.858537	-110.282307	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same gneissic, quartzofeldspathic layering with biotite rich mafic, very magnetic layers; mm scale layering; increasingly mylonitic moving west; half m scale schlieren of amphibolite phyllonite, not magnetic; local pegmatite associated with the kspar granite injections.	main lithology	mylonite	diatexite	biotite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	170	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2156-1	whole-rock lithogeochemistry	Mylonitic orthogneiss.	AL-23-2156-2	whole-rock lithogeochemistry; thin section	Schlieren of amphibolite phyllonite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2157	16-07-2023 14:50:18.922	59.858029	-110.286779	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Protomylonitic magnetic gneiss of previous stations, with m-scale gabbro schlieren with discordant foliation; interpreting this unit as diatexite, and it is possible that the melanosome (biotite-rich mafic layers) are the reason for the magnetic punch; dextral porphyroclast rotation.	main lithology	mylonite	diatexite	biotite	10-20%	hornblende	20-50%	plagioclase	20-50%	buff	gneissic	porphyritic	phaneritic fine (0.5-1mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	108	79	-9999	Taken from gabbro xenolith.	-9999	-9999	-9999	-9999	-9999	AL-23-2157-1	whole-rock lithogeochemistry; thin section	Mylonitic gneissic diatexite paleosome with injections.	AL-23-2157-2	whole-rock lithogeochemistry	Amphibolite schlieren.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2159	16-07-2023 15:25:03.980	59.857107	-110.296843	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	White and grey orthogneiss; less than 10-20% white leucosome component; dextral porphyroclast rotation.	main lithology	mylonite	orthogneiss	biotite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	47	74	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2159-1	whole-rock lithogeochemistry; thin section	Mylonitic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2160	16-07-2023 15:51:54.560	59.849205	-110.302183	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartzite, compositional layering from pelitic to psammitic; weathered out garnets, replaced by biotite and hornblende; appear as hornblende and biotite, randomly oriented porphyry; spotted texture.	main lithology	metatexite	paragneiss	quartz	>50%	plagioclase	20-50%	hornblende	20-50%	dark grey	foliated	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Very fine to cryptocrystaline, compositional layering?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	40	85	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2160-1	whole-rock lithogeochemistry; thin section	Coarser grained paragneiss component; gt-bearing?	AL-23-2160-2	whole-rock lithogeochemistry; thin section	Fine grained paragneiss, potentially bearing microgarnets.	AL-23-2160-3	whole-rock lithogeochemistry	Best displays spotted porphyry.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2161	16-07-2023 16:34:24.219	59.849300	-110.300673	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	What granite is this? Look to geochem.	main lithology	granitoid	granite	hornblende	-9999	-9999	-9999	-9999	-9999	-9999	foliated	equigranular-hypidiomorphic	phaneritic coarse (5-10mm)	Granite composition with recrystallized interlocking grain boundaries; not seeing gneissity; lots of quartz.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	9	90	Lineation weak	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2161-1	whole-rock lithogeochemistry; thin section	Granite.	AL-23-2161-2	whole-rock lithogeochemistry	Granite (cream to buff).	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2163	17-07-2023 14:00:36.010	59.825502	-110.164200	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Transitional zone, older magnetic orthogneiss (white and grey) with leucosome injections of 2.3 Ga granite.	main lithology	metatexite	orthogneiss	magnetite	1-5%	hornblende	20-50%	feldspar	20-50%	grey and white	gneissic	equigranular-xenomorphic	phaneritic very fine (0.1-0.5mm)	Bearing in situ leucosome and melt patches with cm scale black porphyry with apparent right angle cleavage.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	20-50%	biotite	20-50%	buff	massive	-9999	-9999	No notes captured.	VN - Vein	230	85	Foliation moderate	Pegmatite dike foliation parallel.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2163-1	whole-rock lithogeochemistry; thin section	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2164	17-07-2023 14:31:27.131	59.825941	-110.165530	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Largely orthogneiss with magnetic mafic matrix of predominantly hornblende with poor quartz, potential pyroxene (right angle cleavage); biotite and potential sulfides.  Intruded by 2.3 Ga granite and folded with it; in situ partial melting associated with leucosome, generally layer parallel; 85->97.	main lithology	metatexite	orthogneiss	magnetite	1-5%	-9999	-9999	-9999	-9999	-9999	gneissic	migmatitic	-9999	Roughly 70% orthogneiss to 30% 2.3 granite, which is locally pegmatitic. Pegmatite and related granite is potentially nosing into the hinges of major folds, before being further deformed and sheared into a layer parallel style. May reveal timing with respect to deformation.	minor lithology	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	210	90	Foliation strong	Anastomosing and clearly folded.	AXF - Axial fold plane	120	90	-9999	85->097 hinge; e-w trending F3, wrinkling the gneissic fabric.	BD - Fault-Brittle-Ductile	100	90	-9999	Quartz veins coming in along F3 trend; fault/fracture shows offset but cant discern movement; fault is folded very gently, so quartz must be before F3.	AL-23-2164-1	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2165	17-07-2023 15:03:43.651	59.826273	-110.166456	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Predominantly orthogneiss, injected and layered with leucosomal melt probably sourcing from 2.3 Ga granites; leucosome is less abundant here than previous station, increased amount of orthogneiss (10-20% granite leucosome, with hornblende porphyroblasts retrograding to biotite and chlorite, locally pegmatitic) 80% orthogneiss; qt epidote and pegmatite coming in along 130/90.	main lithology	metatexite	orthogneiss	biotite	20-50%	plagioclase	10-20%	hornblende	20-50%	grey and white	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Probable magnetite, very magnetic, bronze coloured sulphide with right angle cleavage, potential cordierite? 10-20% quartz.	minor lithology	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	165	88	Foliation strong	Folded and anastomosing.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2165-1	whole-rock lithogeochemistry; thin section	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2167	17-07-2023 15:30:26.502	59.826418	-110.166053	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous station, but with m-scale layers of pegmatite, locally partially melting out of finer grained granite; and potentially nosing into hinges of major folds, while also layer parallel.	main lithology	metatexite	orthogneiss	magnetite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	dike	granitoid	pegmatite dike	-9999	-9999	-9999	-9999	-9999	-9999	-9999	massive	-9999	pegmatitic	Aplite to pegmatite, folded twice with orthogneiss.	FOL1 - Foliation gen1	-9999	-9999	-9999	-9999	AXF - Axial fold plane	185	90	-9999	Refolded foliation parallel fold.	AXF - Axial fold plane	120	90	-9999	F3 fold, wrinkling layer parallel pegmatite and orthogneiss; basically vertically plunging.	AL-23-2167-1	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2168	17-07-2023 15:51:24.725	59.826036	-110.162996	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Foliated, med grained to pegmatitic.	main lithology	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	220	57	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	FT - Fault Brittle	80	84	-9999	-9999	AL-23-2168-1	whole-rock lithogeochemistry	K-spar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2169	17-07-2023 16:25:08.873	59.830924	-110.164664	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pink and dark grey gneiss, with roughly 75% dark weathering, biotite hornblende plagioclase quartz orthogneiss, extremely magnetic, probable magnetite.  20-30% injections of 2.3 Ga granite, generally layer parallel but some discordance. Layer parallel boudinage of leucosome.	main lithology	metatexite	orthogneiss	magnetite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	177	84	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2169-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2170	17-07-2023 17:16:19.766	59.853012	-110.140722	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Paragneiss; garnet and sillimanite bearing, potential cordierite.  Sulfides and rusty, schisty interlayers.	main lithology	metatexite	paragneiss	garnet	1-5%	sillimanite	5-10%	-9999	-9999	whitish grey	gneissic	equigranular-xenomorphic	phaneritic medium (1-5mm)	Pelitic to psammopelitic metasediments.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	231	84	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2170-1	whole-rock lithogeochemistry; thin section	Pelitic to psammopelitic metasediments; garnet and sillimanite bearing.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2171	19-07-2023 09:38:40.327	59.787609	-110.192299	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Garnets (mm to cm scale), larger ones typically associated with layer parallel in situ partial melting, but not always the case. Roughly 50% paragneiss and 50% Colin Lake leucogranitic injections.	main lithology	metatexite	paragneiss	garnet	5-10%	sillimanite	5-10%	feldspar	20-50%	dark grey	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Fine to very fine grained; metasediments of a dirty, gritty quartz and hornblende/biotite rich matrix. Biotite probably retrograding from hornblende, hornblende and plagioclase likely replacing garnets. Garnets are wrapped by sillimanite+biotite, obvious on weathered surface.	leucosome	granitoid	leucogranite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2171-1	whole-rock lithogeochemistry; thin section	Paragneiss with garnets.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2172	19-07-2023 11:03:43.123	59.781993	-110.195186	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Intermixed, interlayered cm-scale garnet bearing Colin Lake leucogranite with 10cm scale porphyroclasts of feldspar, folded with the paragneiss unit; seeing compositional bands of garnet and sillimamite. To the west, we move into large scale phase of Colin Lake granite; the two lithologies are mylonitized, with ribbon feldspars and quartz; in situ layer parallel leucosome intrudes the sediments and sources from the Colin Lake leucogranite. abundant S-fold asymmetry.	main lithology	mylonite	paragneiss	garnet	5-10%	sillimanite	5-10%	talc	20-50%	grey	protomylonitic	porphyritic	phaneritic fine (0.5-1mm)	Biotite rich, locally rusty schist; compositional layering from pelitic to psammitic; garnets as large as 10cm; locally as protomylonitic porphryoclasts; sample 3 is sillimanite rich pelite with chunk of extremely fine grained pelitic component. The Colin Lake leucogranite is injecting this paragneiss (migmatite) and both are folded, and sheared. Paragneiss features smeared out bands of garnet. Beautiful garnet and sillimanite at eastern part of outcrop. Sinistral C-S-C' fabric given by sigmoids and shear bands. Local cm scale interlayers of amphibolite (very fine-grained).	leucosome	mylonite	leucogranite	garnet	1-5%	feldspar	20-50%	quartz	20-50%	white	protomylonitic	porphyritic	phaneritic coarse (5-10mm)	Garnet bearing.	FOL1 - Foliation gen1	253	90	Foliation intense	Protomylonitic foliation.	AXF - Axial fold plane	50	87	-9999	72->050; hinge line of major folds, whose limbs are dragged into the mylonitic foliation.	-9999	-9999	-9999	-9999	-9999	AL-23-2172-1	whole-rock lithogeochemistry; thin section	Colin Lake granite, mylonite, garnet bearing.	AL-23-2172-2	whole-rock lithogeochemistry; thin section	Rusty mylonitized sediment (pelitic to psammitic, garnets as large as 10cm).	AL-23-2172-3A	whole-rock lithogeochemistry	Sillimanite rich pelite.	AL-23-2172-3B	whole-rock lithogeochemistry	Mylonitic granite.	Alberta Geological Survey
AL-23-2174	19-07-2023 12:55:45.148	59.779695	-110.194772	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Stand corrected about large phase of Colin Lake; everything has been paragneiss with layer parallel injections of Colin Lake leucogranite, locally on the meter scale. Seeing compositional banding and probable layers of aphanitic, mafic volcanics. Still protomylonitic, however, porphyroclasts are much larger (as large as ~0.5m), and display sinistral rotation. Migmatitic nature is obvious; grey laminated pelite is source rock, white leucosome layers make up roughly 30% of the rock, and the black, biotite sillimanite schist with trace garnets represent melanosome (roughly 15-25%), local m scale layers of amphibolite phlyllonite, probably volcanics (sample 2).	main lithology	mylonite	paragneiss	garnet	10-20%	sillimanite	10-20%	biotite	20-50%	alternating shades of grey	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Very fine to med grained, pelitic to psammitic compositional layering; abundant in situ layer parallel partial melting, increasing to the east.	leucosome	granitoid	leucogranite	quartz	20-50%	feldspar	20-50%	garnet	20-50%	white	foliated	migmatitic	phaneritic medium (1-5mm)	Medium grained to pegmatitic.	FOL - Foliation	100	75	Foliation intense	-9999	AXF - Axial fold plane	230	85	-9999	Large m scale S folds of pre existing fabrics, associated axial planar cleavage is weak; hinge is 70->255.	-9999	-9999	-9999	-9999	-9999	AL-23-2174-1	whole-rock lithogeochemistry; oriented thin section	Pelitic to psammitic metaseds. Oriented; 175/73 is fol; L1 (shearing) is 34->175.	AL-23-2174-2	whole-rock lithogeochemistry; thin section	Amphibolite phlyllonite, probably volcanics.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2175	19-07-2023 14:39:01.950	59.777143	-110.197374	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	1100	-9999	5000	-9999	-9999	-9999	Extremely migmatitic, essentially diatexite of source rock (metasediments and volcanics) with pegmatitic leucosome making up 40-60%; 10-20% melanosome bio sil recrystallized garnet schist, and 20-30% grey laminated, qtz rich pelite. Layer parallel leucosome, often pegmatitic. Sample 2 comes from one of two half m wide rusty, schisty biotite pegmatitic quartz melt with secondary uranium mineral staining (yellow), 1100-5000 cps and open along strike and clearly controlled by the foliation, which is folded (can trace around hinge of fold and onwards).  Sample 3 comes from mafic schlieren, which opens up into (?).	main lithology	diatexite	diatexite	quartz	>50%	sillimanite	5-10%	garnet	5-10%	shades of grey and buff (melt)	gneissic	migmatitic	phaneritic medium (1-5mm)	Garnets and sillimanite smeared out into compositional bands; compositional layering, potential layers of quartzite; hottest stuff 5000 cps comes from yellow stained quartz leucosome within layer of biotite pegmatite melt.	schlieren	mafic rocks	amphibolite	biotite	>50%	hornblende	10-20%	plagioclase	10-20%	black with white laminae	schistose	migmatitic	cryptocrystalline (<0.1mm)	Layer parallel leucosome and pegmatite melt.	FOL1 - Foliation gen1	249	70	Foliation intense	Mylonitic foliation, ribboned leucosome and melanosome; associated isoclinal folds axial planar.	AXF - Axial fold plane	264	84	Foliation weak	60->280; axial planar pegmatite; this fold has the mafic volcanic schlieren suspended in pegmatite, with relict foliation/laminae parallel to the long axis of each block, which are rotated about the axis of this fold.	-9999	-9999	-9999	-9999	-9999	AL-23-2175-1	whole-rock lithogeochemistry; thin section	Pegmatite melt, (2000-3000 cps) extremely biotite rich; features m-scale, mm-scale laminated mafic volcanics suspended in pegmatite melt.	AL-23-2175-2	whole-rock lithogeochemistry	Rusty, schisty bt- pegmatitic qtz melts, ~3000 cps.	AL-23-2175-3	whole-rock lithogeochemistry	Amphibolite schlieren.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2176	19-07-2023 15:41:57.747	59.777709	-110.198512	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Transitional contact into TBC pink granite gneiss, foliation parallel 230/80.	main lithology	gneiss	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2177	19-07-2023 15:59:40.474	59.779098	-110.199411	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Found trench, hosted in protomylonitic k-spar granite gneiss with biotite chlorite rich matrix, with potential smeared out compositional bands of garnets and layers. Sample taken from 1m wide trench of rusty leucosome, granite to straight quartz; m-scale leucosome of Colin Lake granitoid composition shows yellow uranium staining, prominent on weathered surface; mylonitized leucosome; seems to be a contact with TBC 2.3 Ga granite running foliation parallel.	main lithology	diatexite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Uranium rich leucogranite along contact between biotite granite gneiss and paragneiss, also on other side. Foliation is very interesting through this traverse, need to key in on this. Lots of structural data to interpret.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	155	85	-9999	Changed since last station.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2177-1	whole-rock lithogeochemistry	Sample taken from 1m wide trench of rusty leucosome, granite to straight quartz.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2178	21-07-2023 11:20:39.759	59.770114	-110.227620	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mylonitic orthogneiss with layer parallel leucogranitic injections of pink alkali feldspar granite.  Magnetic, locally massive mafic matrix, with probable magnetite.  M-scale xenoliths of gabbroic amphibolite. Textbook S-folds, rootless, best displayed by mafic schlieren.	main lithology	metatexite	orthogneiss	biotite	20-50%	quartz	10-20%	plagioclase	20-50%	greyish brown to buff	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Contains clear mafic schlieren of amphibolite, migmatite; bears hornblende retrograding to biotite, probable magnetite, and silver to bronze coloured sulphides. Leucosome is mainly alkali feldspar and quartz, and contains black, conchoidal quartz which is typical of the 2.3Ma granite. Roughly 60-70% orthogneiss compared to 20-35% leucosome.	schlieren	mafic rocks	amphibolite	hornblende	20-50%	biotite	20-50%	plagioclase	10-20%	dark grey to black	foliated	migmatitic	phaneritic coarse (5-10mm)	Hornblende retrograding through to chlorite, very green.	FOL2 - Foliation gen2	237	88	Foliation intense	Anastomosing and dramatically folded, this is the general trend; isoclinal folds are generally parallel but often discordant especially around schlieren.	AXF - Axial fold plane	270	90	Foliation weak	65->275; hinge line of dominant phase of folding. Drag folds along axial plane; abundant S-fold asymmetry; rusty fractures running 105/vertical, almost axial planar.	FOL - Foliation	175	85	Foliation strong	Orientation of relict foliation within gabbro enclaves.	AL-23-2178-1	whole-rock lithogeochemistry; thin section	Mylonitic orthogneiss.	AL-23-2178-2	whole-rock lithogeochemistry	Amphibolite gabbro, showing mixing with orthogneiss (schlieren).	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2179	21-07-2023 12:10:42.492	59.769493	-110.227277	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	2	-9999	400	-9999	-9999	-9999	Increasing amount of pink weathering moving east; background cps of 2-400, similar to previous station; roughly 50-55% orthogneiss, 45-50% leucosome; mylonitic fabric is folded; is it the same? Amphibolite interlayers (more likely biotite schist melanosome) are abundant; shearing along fold axial planes, etc. Massive, oval shaped lens of epidote (very coarse grained, similar to what we saw in mylonite gabbro xenoliths), with finer grained margin (2 cm thick).	main lithology	metatexite	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	buff to grey	gneissic	migmatitic	-9999	No notes captured.	leucosome	gneiss	alkali-feldspar granite	alkali-feldspar	20-50%	quartz	20-50%	biotite	5-10%	buff	gneissic	migmatitic	phaneritic medium (1-5mm)	Fine to pegmatitic, interlayered with orthogneiss (paleosome?), often boudined.	FOL2 - Foliation gen2	225	85	Foliation intense	Folded, anastomosing dominant fabric.	AXF - Axial fold plane	-9999	-9999	-9999	68->285; hinge of dominant phase of folding, associated with axial planar kspar granite to pegmatite. Refolding early set.	AXF - Axial fold plane	340	83	Foliation weak	65->165; hinge of potential early set of folds; axial planar relict foliation is overprinted by S-main, weak but traceable, with axial planar granitic to pegmatitic leucosome.	AL-23-2179-1	whole-rock lithogeochemistry; thin section	Orthogneiss migmatite with leucosome intermixed.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2180	21-07-2023 12:56:49.444	59.767689	-110.224479	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	800	-9999	-9999	-9999	Seeing lithologic change corresponding to transition into lower magnetics. Lots of pink granite with very little mafic content; blotchy, buff weathering and containing; medium grained to pegmatitic; cm scale qtz and plag porphyry.	main lithology	diatexite	granite	quartz	20-50%	alkali-feldspar	10-20%	biotite	5-10%	yellowish buff	foliated	porphyritic	phaneritic coarse (5-10mm)	Locally massive; associated with higher background cps (500-800) pretty much everywhere; mafic minerals are magnetic; probably biotite retrograding from hornblende, associated potentially with sulfides and magnetite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	235	85	Foliation weak	-9999	AXF - Axial fold plane	115	85	-9999	80->290; dominant hinge of folds; associated axial planar S2 cleavage.	VN - Vein	310	90	-9999	Quartz leucocratic melt.	AL-23-2180-1	whole-rock lithogeochemistry	Pink leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2181	21-07-2023 13:07:46.516	59.767369	-110.223626	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mixed orthogneiss and leucosome; diatexite, larger component of 2.3 Ga granite leucosome than orthogneiss; seeing rafts of orthogneiss within granite; mylonitic; plagioclase and hornblende +/- biotite alternating with kspar and quartz; mm to cm scale banding; gneissic; no longer magnetic. Possibly interpreting the continuation of the sediment package with white leucogranite injections, further intruded by the pink leucogranite. Ample schlieren and melanosome.	main lithology	gneiss	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Leucogranite is fine to medium grained and massive and is both foliation parallel (coming in along planes of weakness) and also axial planar to main folds. Local pegmatite. Paleosome is proto- to meso-mylonitized.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2181-1	whole-rock lithogeochemistry; thin section	Mylonitic orthogneiss - plagioclase and hornblende and biotite alternating with kspar and quartz.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2184	21-07-2023 18:00:29.071	59.756766	-110.108356	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	1000	7000	7.4	44	7.4	Trench location; up to 7000 cps; took sample of rusty peg schist, porphyroblastic granodiorite with cm scale kspars. Background of 1000 cps in main granodiorite stuff. It is interlayered, and appears to be melting out of med-grained granodiorite like we saw at the last station, which would make this diatexite dominated by pegmatitic leucosome (in-situ), which becomes increasingly dominated by partial melting moving west. Unfortunately could not push further into uranium/magnetic high due to time conflict and incoming thunder storm. Extremely interesting prospect for future work. Assay #77 - U:406 ppm Th:44 ppm K:7.4%.	main lithology	dioritoid	diatexite	alkali-feldspar	20-50%	biotite	20-50%	quartz	5-10%	dark grey	foliated	migmatitic	phaneritic coarse (5-10mm)	Coarse to very coarse; difficult to interpret; it could be a protomylonized granodiorite with cm-scale clasts of plagioclase feldspar, or, it could be a full on diatexite, with intermediate schlieren suspended within pegmatitic melt, in which case the feldspars are more likely K-spar within biotite rich matrix. Didn't have a lot of time to figure it out. Injected by Colin leucogranite, with consistent yellow secondary uranium mineral staining. The unit is extremely rusty to the west, where we start seeing m-scale xenoliths of amphibolite. These enclaves may be schlieren suspended in melt. Need to sort out samples here. Mineralization is hosted within a m-scale fault, containing a finer grained, quartzofeldspathic granodiorite in contact with nearly pure quartz, with rusty interlayers (amphibolite?).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	150	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2184-1	whole-rock lithogeochemistry; thin section	Granodiorite.	AL-23-2184-2	whole-rock lithogeochemistry; thin section	Rusty pegmatitic schist (~3000 cps).	AL-23-2184-3A; AL-23-2184-3B	whole-rock lithogeochemistry	Sample 3A is biotite schist, sample 3B is coarse-grained qtz pegmatite.	AL-23-2184-4	whole-rock lithogeochemistry	Mafic xenolith.	Alberta Geological Survey
AL-23-2185	22-07-2023 08:53:52.974	59.699455	-110.457744	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	200	-9999	10000	15.8	230	15.8	This looks like a dirty melted leucocratic sediment, ultra strong.  Migmatite. Majority of rock is dark grey to black weathering pelitic rock with leucocratic layering on mm to cm scale.  Both the main lithology and the in situ leucocratic pegmatite are folded together.  Typically the dark unit reads about 200 background cps; anywhere the scint hovers over the leucosome, shoots up to at least 600-700 cps. 70-80% biotite schist, and the rest is the leucosome, often as lenses in the host rock. Assays #77 and #78 - K: 7.4% U: 213.2ppm Th : 651.4 ppm; 10000 cps; second assay a few cms over, in higher counts reads 15.8% K, 230 ppm U, and 585.4 ppm Th.	main lithology	metatexite	protomylonite	biotite	>50%	feldspar	10-20%	quartz	10-20%	dark grey to black	schistose	migmatitic	phaneritic very fine (0.1-0.5mm)	Biotite hornblende schist, not magnetic; locally the grey, recrystallized rock that makes up the paleosome is extremely sheared, and phyllonitized, with m-scale lens of leucogranite suspended in the biotite schist; if this schist represents melanosome, then this is more likely a diatexite; if the schist is recrystallized, sheared paleosome then it is metatexite. Seeing abundant enclaves/schlieren of amphibolite of varying composition, from dark grey to hornblende green, typically boudined/sheared. Rusty, biotite rich layers with porphyroclasts of the leucosome, or enveloping the leucosome may be melanosome, and is where the 10000 cps sample came from.	leucosome	granitoid	tonalite	plagioclase	>50%	quartz	20-50%	chlorite	1-5%	white	massive	migmatitic	pegmatitic	Probable sulphides and patches of biotite chlorite; assuming plagioclase due to 0% K readouts on scint. This lith has yellow alteration abundant on weathered surface. Assay #80 - U; 15.1 ppm; Th 3.1 ppm; K 0%.	FOL - Foliation	31	87	Foliation strong	-9999	AXF - Axial fold plane	69	86	Foliation weak	85->246; hinge, axial planar S2 cleavage associated is weak.	AXF - Axial fold plane	207	85	Foliation moderate	86->210; hinge of F2 folds, a few meters to the east of prev.	AL-23-2185-1	whole-rock lithogeochemistry	Chips of hot zone (dirty melted leucocratic sediment, ultra strong, migmatitic).	AL-23-2185-2	oriented thin section	Oriented biotite hornblende schist.	AL-23-2185-3	whole-rock lithogeochemistry	Leucosomal component.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2186	22-07-2023 10:36:24.785	59.700489	-110.458140	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	0.9	9	0.9	Sillimanite hornblende phyllonite, with multiple cm scale porphyroclasts of qtz and feldspar, rounded and weathering out of extremely mafic matrix.  Full on ribbon mylonite, with ribboned flatted feldspars and qtz leucosomes/clasts. Assay for this is 0.9% K, 1.4 ppm U, 9 ppm Th.	main lithology	schist	phyllonite	actinolite	-9999	epidote	-9999	hornblende	-9999	greenish grey	schistose	porphyritic	phaneritic very fine (0.1-0.5mm)	Clinozoisite and glaucophane picked up by HALO; also bears sillimanite (10-20%); definite chlorite (potentially mistaking chlorite here for sillimanite). Some type of para-amphibolite? yellow staining; 80% actinolite phyllonite here; the leucosome has 2% K, 14.4 ppm U, 129.2 ppm Th	minor lithology	mylonite	quartzite	-9999	-9999	-9999	-9999	-9999	-9999	white to buff	mylonitic	migmatitic	-9999	Highly strained, 1.5m wide layer of apparent mylonitized quartzite.	FOL - Foliation	67	75	Foliation intense	-9999	AXF - Axial fold plane	150	82	-9999	67-> 145; hinge.	LINM - Lineation mineral	-9999	-9999	-9999	45->30; strong stretching lineation.	AL-23-2186-1	whole-rock lithogeochemistry; thin section	Phyllonite.	AL-23-2186-2	whole-rock lithogeochemistry	Mylonitized quartzite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2187	22-07-2023 12:53:04.309	59.696461	-110.469811	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	1000	-9999	0.8	253.4	0.8	Aplitic to granitic dikes have background cps of 1000. Assay; K: 0.8% U: 19.6 ppm; Th: 253.4 ppm; Assay #83; dikes coming in at 060/83 (orientation). 20-25% dike, rest is high strain mafic migmatite, orthogneiss? dikes are massive, must be later. Pegmatite phase associated with lower counts (~700) and are even later, cross cutting clearly the older migmatite.  Older grey package has layer parallel leucosome, not super abundant but the same thing we have been seeing all day, i.e. yellow staining.	main lithology	gneiss	metatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	dike	granitoid	aplite dike	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	55	88	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2187-1	whole-rock lithogeochemistry	Host rock migmatitic mess with gabbroic weathering.	AL-23-2187-2	whole-rock lithogeochemistry; thin section	Hot aplite dike, 2000 cps.	AL-23-2187-3	whole-rock lithogeochemistry	Migmatite with small aplite veinlets.	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2188	22-07-2023 16:46:46.693	59.766146	-110.090192	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Trench, white leucogranite layer parallel with diorite looking unit which is similar to what was sampled west of Cherry Lake yesterday. The leucosome (or injected granite) has lots of biotite in it. 80% at least for leucogranite, then 20% diorite or granodiorite gneiss host rock, which shows partial melting.	main lithology	metatexite	metatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	220	88	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2188-1	whole-rock lithogeochemistry	Granite/leucosome.	AL-23-2188-2	whole-rock lithogeochemistry	Granodiorite gneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
AL-23-2189	22-07-2023 17:41:26.319	59.759530	-110.089593	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	37000	17.3	75.8	17.3	Drill core, several boxes worth right next to 37000 cps on scint.  K: 17.3%%, U: 2248ppm; 75.8ppm Th -- rushed station.	main lithology	mylonite	granite	biotite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	diatexite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AL-23-2189-1	whole-rock lithogeochemistry	From within trench, next to drill core. Northerly trending shear zone. Leucosomal biotite granite melt; high cps; potentially bearing garnets.	AL-23-2189-2	whole-rock lithogeochemistry	From within trench, next to drill core. Quartzitic ultramylonite yielding several thousand cps.	AL-23-2189-3	whole-rock lithogeochemistry	From within trench, next to drill core. Biotite granite host rock; High cps.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1001	22-06-2023 16:30:15.897	59.813567	-111.049839	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.5	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Grey to brown gneissic rock. Quite mixed with abundant blue quartz and knots that appear to contain sillimanite. Abundant garnet. MS -0.5. The east part of the outcrop has schistose material. There is a 20cm pegmatitic granite that cuts the gneissosity.	main lithology	mylonite	paragneiss	garnet	10-20%	-9999	-9999	-9999	-9999	grey	gneissic	-9999	phaneritic coarse (5-10mm)	No notes captured.	unknown	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic very coarse (10-50mm)	No notes captured.	FOL1 - Foliation gen1	54	79	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1001-1	whole-rock lithogeochemistry; thin section	Two pieces, primary unit (garnet paragneiss).	LL-23-1001-2	whole-rock lithogeochemistry	Sample of schistose (garnet paragneiss) component at east end of outcrop.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1002	23-06-2023 08:58:50.501	59.809268	-111.050674	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Traverse directly across the lake from our camp. Burned area with some lichen. 60% of outcrop is pink granite and 40% is a grey gneiss with enclaves of biotite rich material and magnetite. Isoclinal folding is present. The gneiss is likely granulite grade.	main lithology	gneiss	orthogneiss	hypersthene	1-5%	-9999	-9999	-9999	-9999	pink to grey	gneissic	-9999	phaneritic coarse (5-10mm)	No notes captured.	schlieren	mafic rocks	mafic schist	magnetite	<1%	biotite	20-50%	-9999	-9999	dark grey	schistose	-9999	-9999	No notes captured.	FOL - Foliation	15	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1002-1	whole-rock lithogeochemistry; thin section	Mafic component; magnetic.	LL-23-1002-2	whole-rock lithogeochemistry; thin section	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1003	23-06-2023 10:11:23.183	59.809096	-111.051431	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same gneiss as at the previous outcrop with some pink potassium alteration.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1004	23-06-2023 10:18:15.359	59.809337	-111.052640	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large outcrop ridge. There is some chlorite retrogression in places.	main lithology	gneiss	paragneiss	garnet	5-10%	-9999	-9999	-9999	-9999	grey to pink	foliated	equigranular	phaneritic medium (1-5mm)	Garnets up to 3 cm in size. Rock is equigranular with 20% biotite, 20% garnet, 40% quartz, 10-20% feldspar and possible sillimanite.	vein	-9999	-9999	quartz	>50%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	There are numerous quartz veins that parallel the gneissosity.	FOL - Foliation	22	86	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1005	23-06-2023 10:50:19.806	59.809562	-111.052604	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Leucogranite pegmatite that is 80cm wide cross-cuts the paragneiss here. The pegmatite contains large muscovite booklets.	dike	granitoid	pegmatite	muscovite	1-5%	alkali-feldspar	>50%	Quartz	35-40%	-9999	-9999	-9999	-9999	K-spar crystals are up to 10cm in length.	main lithology	gneiss	paragneiss	garnet	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Host rock is paragneiss. Isoclinal folding is visible here.	IGC - Contacts	74	86	-9999	Orientation of pegmatite.	LINF - Lineation fold	235	15	-9999	Isoclinal fold.	-9999	-9999	-9999	-9999	-9999	LL-23-1005-1	whole-rock lithogeochemistry	Pegmatite (cutting paragneiss) with muscovite books.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1006	23-06-2023 11:22:14.637	59.809143	-111.054329	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strain gradation is visible. We see a paragneiss that transitions into a schistose ribbon mylonite. The outcrop is rounded and there is a "moat" of water on the east side that likely coincides with a major fault structure.	main lithology	mylonite	ultramylonite	chlorite	<1%	-9999	-9999	-9999	-9999	brown green	-9999	-9999	-9999	Chlorite alteration occurs as pods. Lots of injected quartz (80%) along the east side of the unit.	main lithology	gneiss	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	220	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1007	23-06-2023 11:47:57.787	59.809553	-111.056205	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	50	-9999	-9999	-9999	-9999	-9999	-9999	There appears to be a transition here into a migmatite that has not been retrogressed by the shear zone. The rock is extremely magnetic here with a MS >50. It will be important to look at a thin section of this rock to determine the grade.	main lithology	diatexite	diatexite	garnet	<1%	magnetite	5-10%	hypersthene	1-5%	grey to pink	foliated	migmatitic	-9999	Recessive spots that look to be hypersthene.	sheet	metatexite	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Pegmatitic leucosome.	FOL - Foliation	200	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1007-1	whole-rock lithogeochemistry; thin section	Representative migmatite, extremely magnetic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1008	23-06-2023 12:47:30.178	59.809623	-111.059641	Internal GPS	Alex MacNeil	Russell Hartlaub	10	-9999	50	-9999	-9999	-9999	-9999	-9999	-9999	Continuous outcrop from the last station. Uniform pink granitic migmatite that appears spotted. There are weathered out minerals that should be identified. MS ranges from 10 to 50. There are some pegmatitic melt zones that parallel foliation.	main lithology	diatexite	diatexite	magnetite	<1%	hypersthene	1-5%	-9999	-9999	pink	layered	migmatitic	-9999	Recessive spots that may be hypersthene, check thin section. There are some grey schlieren type layers.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	25	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1009	23-06-2023 13:18:46.663	59.810134	-111.064363	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mushrooms (Morels) in burnt marsh area. We passed through a swamp to get to this outcrop.	main lithology	granitoid	granite	plagioclase	20-50%	biotite	1-5%	-9999	-9999	white	foliated	equigranular	phaneritic coarse (5-10mm)	There is a blue quartz in this rock that looks a lot like cordierite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	210	59	-9999	-9999	VN - Vein	310	78	-9999	This vein cuts through the granite.	-9999	-9999	-9999	-9999	-9999	LL-23-1009-1	whole-rock lithogeochemistry; thin section	White granite.	LL-23-1009-2	whole-rock lithogeochemistry	White granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1010	23-06-2023 14:10:33.396	59.810615	-111.066860	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous granite, but contains trace garnet.	main lithology	granitoid	granite	biotite	5-10%	plagioclase	20-50%	garnet	<1%	white	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	30	62	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1010-1	whole-rock lithogeochemistry; thin section	White granite with trace garnet.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1011	23-06-2023 14:31:51.394	59.811036	-111.069050	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	This is a huge outcrop of white granite.	main lithology	granitoid	granite	biotite	5-10%	chlorite	<1%	garnet	<1%	white	foliated	equigranular	phaneritic medium (1-5mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	355	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1012	23-06-2023 14:52:53.568	59.809501	-111.070311	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same white granite as previous with traces of epidote. Quartz 30%. Measurements - MS 0.15.	main lithology	granitoid	granite	biotite	5-10%	epidote	<1%	plagioclase	20-50%	white	foliated	equigranular	phaneritic coarse (5-10mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	30	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1012-1	whole-rock lithogeochemistry; thin section	White granite with trace epidote.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1013	23-06-2023 15:20:11.118	59.809065	-111.067498	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.15	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Low mag susceptibility, equigranular white to pink granite. This area is burned but there is still lichen. Measurements - MS 0.15.	main lithology	granitoid	granite	biotite	1-5%	plagioclase	20-50%	-9999	-9999	white and pink	foliated	equigranular	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	20	72	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1014	23-06-2023 16:05:47.022	59.808919	-111.060171	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	We have crossed back east into the spotted migmatite. There are pegmatitic leucosomes as well as a mafic layer that may represent a metamorphosed dike.	main lithology	diatexite	diatexite	magnetite	<1%	hypersthene	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	Pegmatitic leucosome. Spotted rock with recessive mineral that is likely hypersthene.	schlieren	mafic rocks	mafic gneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	196	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1014-1	whole-rock lithogeochemistry; thin section	Spotted migmatite. Check the Thin section for metamorphic minerals and grade. Is there hypersthene in this rock?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1015	23-06-2023 16:46:39.539	59.809118	-111.053054	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Small pegmatite (40cm wide) that cuts through the paragneiss. The paragneiss seems quartz rich here and very well foliated.	main lithology	gneiss	paragneiss	garnet	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	dike	granitoid	pegmatite dike	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	11	86	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1015-1	whole-rock lithogeochemistry; thin section	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1016	24-06-2023 08:56:24.401	59.799166	-111.036703	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	6	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Traverse east of Leland Lake. We start in our typical "orthogneiss" unit. This unit contains 10% mafic enclaves of medium grained amphibolite. The actual original rock unit is difficult to determine as the gneiss is fairly heterogeneous. Geochemical differentiation may be helpful. Measurements - MS 6.	main lithology	gneiss	orthogneiss	hornblende	5-10%	magnetite	<1%	-9999	-9999	pink to white	gneissic	-9999	phaneritic coarse (5-10mm)	No notes captured.	enclave	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	greenish black	-9999	equigranular	phaneritic fine (0.5-1mm)	No notes captured.	FOL - Foliation	21	65	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1017	24-06-2023 09:15:29.003	59.801078	-111.037901	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	1.1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	The main unit is the typical heterogeneous "orthogneiss" that contains 10% mafic schlieren (mafic enclaves) of unknown origin. The second unit is leucocratic k-feldspar granite that makes up 50% of the outcrop and appears to be intrusive into the gneiss. Measurements - MS 1.1.	main lithology	gneiss	orthogneiss	hornblende	5-10%	-9999	-9999	-9999	-9999	pink to white	gneissic	-9999	phaneritic coarse (5-10mm)	No notes captured.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	porphyritic	phaneritic coarse (5-10mm)	K-feldspar phenocrysts.	FOL - Foliation	25	82	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1017-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1018	24-06-2023 09:43:52.049	59.798734	-111.034887	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	0.049	-9999	-9999	-9999	-9999	-9999	-9999	-9999	K-feldspar crystals up to 6cm in this granite. MS - 0.049 (lower than the gneiss).	main lithology	granitoid	granite	alkali-feldspar	-9999	biotite	1-5%	chlorite	1-5%	white with large pink kfsp	foliated	porphyritic	phaneritic coarse (5-10mm)	Less magnetite than last station; hematite or Mg oxide.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	50	79	Foliation weak	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1018-1	whole-rock lithogeochemistry	K-spar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1019	24-06-2023 10:13:56.970	59.798166	-111.033461	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same megacrystic granite here but it has red hematitic staining. There were numerous boulders between here and the previous outcrop.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1020	24-06-2023 10:27:42.407	59.796359	-111.028318	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	12.2	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large ridge of uniform outcrop. Pink megacrystic granite with trace magnetite. MS 12.2.	main lithology	granitoid	granite	magnetite	<1%	-9999	-9999	-9999	-9999	pink to white	foliated	porphyritic	phaneritic coarse (5-10mm)	Megacrysts are grey here. Is this microcline? There is 25% quartz and 30% plag in matrix. The rock is foliated, but there are no xenoliths here.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	40	73	-9999	-9999	VN - Vein	311	76	-9999	Quartz; subvertical orthogonal veins (45 degree second set).	VN - Vein	161	25	-9999	Quartz veins, lineations at 306 and 180.	LL-23-1020-1	whole-rock lithogeochemistry; thin section	Pink megacrystic granite with trace magnetite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1021	24-06-2023 11:29:35.758	59.798166	-111.033461	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge ridge of outcrop. Similar to previous with more joints and hematite staining. Well exposed rock. There are a few strained xenoliths at the bottom of the hill.	main lithology	granitoid	granite	chlorite	<1%	biotite	1-5%	magnetite	<1%	pink to white	foliated	porphyritic	phaneritic coarse (5-10mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	20	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1021-1	whole-rock lithogeochemistry; thin section	Pink megacrystic granite, hematite staining.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1022	24-06-2023 11:53:26.024	59.796831	-111.027448	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	24.5	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Approximately 40% of the outcrop is mafic xenoliths and enclaves. Amphibolite and dioritic. There are thin pegmatitic melt patches in the foliation. Looks to be a migmatite in places. MS 24.5.	main lithology	gneiss	orthogneiss	hornblende	5-10%	magnetite	<1%	-9999	-9999	pink to white	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	equigranular	phaneritic coarse (5-10mm)	Granite sheets (10-40 cm) within gneiss, parallel to gneissosity. This is likely the Arch Lake granite as we are near the intrusive contact.	FOL - Foliation	205	76	-9999	-9999	BD - Fault-Brittle-Ductile	86	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1022-1	whole-rock lithogeochemistry	Magnetic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1023	24-06-2023 12:47:55.073	59.791932	-111.024505	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Lots of xenoliths here. This was our lunch spot with poor weather and rain coming in.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1023-1	whole-rock lithogeochemistry	White and leucocratic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1024	24-06-2023 12:57:13.328	59.798166	-111.033461	Internal GPS	Alex MacNeil	Russell Hartlaub	0	-9999	0.9	-9999	-9999	-9999	-9999	-9999	-9999	This is a large ridge of outcrop. 50% is a very heterogeneous gneiss with numerous xenoliths, 50% is a white clean leucogranite. Measurements - MS  0.9 (gneiss); MS 0 (leucogranite).	main lithology	gneiss	orthogneiss	hornblende	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	quartz-rich granitoid	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Leucogranite.	FOL - Foliation	198	82	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1024-1	whole-rock lithogeochemistry	White leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1025	24-06-2023 13:23:50.250	59.798166	-111.033461	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	210	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1025-1	whole-rock lithogeochemistry	Mafic amphibolite dike.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1026	24-06-2023 13:53:34.753	59.797307	-111.023788	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	190	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1026-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1027	24-06-2023 14:12:32.891	59.800248	-111.022405	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	1.7	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pink Augen gneiss. Strong mylonitic bands in places. 10-20% mafic schlieren. There are a number of Z folds here. Measurements - MS 1.7.	main lithology	gneiss	orthogneiss	alkali-feldspar	20-50%	chlorite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	25	75	-9999	-9999	LINF - Lineation fold	215	39	-9999	Z-fold.	-9999	-9999	-9999	-9999	-9999	LL-23-1027-1	whole-rock lithogeochemistry; thin section	Pink augen orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1028	25-06-2023 10:03:41.983	59.937445	-110.994802	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	-9999	North portion of Leland Lake. Traverse by air strip and cabins.	main lithology	mylonite	mesomylonite	biotite	1-5%	chlorite	<1%	magnetite	<1%	pink	foliated	-9999	phaneritic medium (1-5mm)	Granite mylonite. There are mm scale bands of ribbon mylonite. K-spar porphyroclasts are common. MS 2.0 There are a few deformed mafic layers but it mostly appears to be a granite or granite gneiss originally.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	190	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1028-1	whole-rock lithogeochemistry	Granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1029	25-06-2023 10:25:37.097	59.936937	-110.994119	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mylonitic granite with amphibolite, looks like dikes.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic medium (1-5mm)	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	dark grey	foliated	-9999	-9999	No notes captured.	FOL - Foliation	185	72	-9999	-9999	VN - Vein	320	87	-9999	Quartz vein.	-9999	-9999	-9999	-9999	-9999	LL-23-1029-1	whole-rock lithogeochemistry	Mylonitic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1030	25-06-2023 10:48:30.367	59.936336	-110.992447	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	The main unit is mylonitic granite (60%). There is also 20% amphibolite and 20% biotite rich schlieren. Original rocks could be our heterogeneous orthogneiss.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	180	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1031	25-06-2023 11:02:09.195	59.935405	-110.991155	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Granite mylonite with no mafic layers or xenoliths. Much more uniform than the last outcrop.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic medium (1-5mm)	Granite mylonite; no mafic layers/sheets.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	174	84	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1031-1	whole-rock lithogeochemistry	Granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1032	25-06-2023 11:16:09.123	59.934579	-110.990090	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Uniform outcrop from the last station. All granite with no dikes or veins. Strong mylonitic fabric to the rock. Descending down of the hill we do see some mafic xenolith/dismembered dikes.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic medium (1-5mm)	Granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	174	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1033	25-06-2023 11:35:58.988	59.933750	-110.987574	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	1.7	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Very lichen covered outcrop. Small and in valley. Mylonitic granite is the same as previous outcrop. Measurements - MS 1.7.	main lithology	mylonite	mesomylonite	biotite	1-5%	chlorite	<1%	magnetite	<1%	pink	foliated	-9999	phaneritic medium (1-5mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1033-1	whole-rock lithogeochemistry	Mylonitic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1034	25-06-2023 11:55:00.241	59.933675	-110.984815	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	This outcrop contains lots of large grey k-spar porphyroclasts.	main lithology	mylonite	protomylonite	alkali-feldspar	20-50%	magnetite	<1%	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Kfsp Porphyroclasts. 30%? plag, 20% quartz, trace magnetite and chlorite. Biotite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	350	84	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1034-1	whole-rock lithogeochemistry	Granite mylonite with lots of large grey k-spar porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1035	25-06-2023 12:18:54.744	59.933195	-110.982419	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge outcrop area. Hematite staining locally. White to pale pink granite.	main lithology	mylonite	protomylonite	biotite	1-5%	magnetite	<1%	-9999	-9999	pink	-9999	-9999	-9999	Very uniform.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	168	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1035-1	whole-rock lithogeochemistry; thin section	Mylonitic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1036	25-06-2023 13:13:59.185	59.931967	-110.980119	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Porphyroclastic, granite, arch lake type, uniform with no xenoliths. Quite felsic here.	main lithology	mylonite	protomylonite	magnetite	<1%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	344	86	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1037	25-06-2023 13:40:23.757	59.929821	-110.976751	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Large outcrop after swamp. Pink protomylonite.	main lithology	mylonite	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	342	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1037-1	whole-rock lithogeochemistry	Pink granite protomylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1038	25-06-2023 14:00:29.331	59.931477	-110.973725	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mapped as Unit 31 by Godfrey but no aluminosilicates. This is a granite with 10% K-spar porphyroclasts. There are pink potassic leucocratic zones up to 20m across. More biotite here than previous outcrops.	main lithology	mylonite	protomylonite	biotite	10-20%	chlorite	<1%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	330	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1038-1	whole-rock lithogeochemistry	Protomylonite granite with 10% K-spar porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1039	25-06-2023 14:21:35.602	59.932986	-110.971901	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	71.9	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Increased biotite here 15-20%. MS 71.9 with visible magnetite. There are some small pegmatite melt pods between boudinaged layers.	main lithology	mylonite	protomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	pink and white	-9999	-9999	-9999	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	342	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1039-1	whole-rock lithogeochemistry; thin section	Amphibolite sample, very high mag susceptibility.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1040	25-06-2023 14:57:07.494	59.934717	-110.973855	Internal GPS	Alex MacNeil	Russell Hartlaub	30	-9999	40	-9999	-9999	-9999	-9999	-9999	-9999	High mag susceptibility (MS 30 to 40). Large porphyroclasts here that appear black to dark grey in colour. No visible mafic xenoliths or enclaves.	main lithology	mylonite	protomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	144	74	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1041	25-06-2023 15:22:44.278	59.935614	-110.977073	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quick stop- heavy lichen cover. Same as previous outcrop.	main lithology	mylonite	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1042	25-06-2023 15:35:48.488	59.935822	-110.980957	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Almost 100% lichen cover. Same as previous with large black to grey feldspar porphyroclasts.	main lithology	mylonite	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Trace magnetite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	170	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1042-1	whole-rock lithogeochemistry; thin section	Granite protomylonite with large black to grey feldspar porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1043	25-06-2023 15:58:29.204	59.936914	-110.984953	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Grey feldspar porphyroclasts are abundant. Same as previous outcrops.	main lithology	mylonite	protomylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	175	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1043-1	whole-rock lithogeochemistry	Granite protomylonite with abundant grey feldspar porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1044	26-06-2023 09:08:53.672	59.830096	-111.027035	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	2.1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Lake shore just north of the "rapids" in the middle of Leland Lake. 5m wide gneissic bands. 20% of the outcrop is mafic layers that are locally disrupted with MS - 2.1. 80% of the outcrop is quartzofeldspathic material that is leucocratic.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	-9999	biotite	20-50%	magnetite	<1%	-9999	-9999	grey	foliated	-9999	-9999	Additional amphibole sheets.	FOL - Foliation	188	75	-9999	-9999	SH - Shear Ductile	100	72	-9999	Dextral.	LINF - Lineation fold	275	60	-9999	Open; late generation (S1).	LL-23-1044-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1045	26-06-2023 09:32:24.137	59.829841	-111.027812	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	0.07	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Clean outcrop. Very strongly foliated pink to white leucocratic granite with 5-10% biotite and chlorite that may be replacing something else. Less than 5% mafic inclusions/layers. MS 0.07. There are brittle ductile shears.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink to white	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FT - Fault Brittle	30	69	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1045-1	whole-rock lithogeochemistry	Pink to white leucocratic granite with 5-10% biotite and chlorite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1046	26-06-2023 10:19:39.012	59.831598	-111.028082	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	0.37	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Approximately 70% granite mylonite and 30% intermediate band (2m wide) that contains biotite, chlorite, garnet, graphite and pyrite with MS 0.37.	main lithology	mylonite	mesomylonite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	phaneritic coarse (5-10mm)	No notes captured.	main lithology	schist	intermediate schist	graphite	<1%	garnet	<1%	biotite	20-50%	-9999	schistose	-9999	phaneritic medium (1-5mm)	Additional minerals observed: pyrite, chlorite, other sulphides (?), quartz.	FOL - Foliation	41	82	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1046-1	whole-rock lithogeochemistry; thin section	Granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1047	26-06-2023 10:59:47.962	59.831342	-111.031521	Internal GPS	Courtney Reimert	Russell Hartlaub	2	-9999	3	-9999	-9999	-9999	-9999	-9999	-9999	Spotted orthogneiss with garnet(?) replaced by biotite. 40% of the outcrop is mafic inclusions and layers (amphibole schist), many of which are rotated and have MS 2 to 3.	main lithology	diatexite	diatexite	-9999	-9999	-9999	-9999	-9999	-9999	pink to grey	foliated	-9999	phaneritic coarse (5-10mm)	Garnet?	main lithology	mafic rocks	amphibolite	magnetite	<1%	-9999	-9999	-9999	-9999	dark grey	-9999	equigranular	phaneritic fine (0.5-1mm)	No notes captured.	FOL - Foliation	24	64	-9999	-9999	SH - Shear Ductile	250	50	-9999	Dextral.	-9999	-9999	-9999	-9999	-9999	LL-23-1047-1	whole-rock lithogeochemistry; thin section	Spotted migmatitic orthogneiss with garnet?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1048	26-06-2023 11:47:25.777	59.836679	-111.023675	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	7	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Spotted migmatite with 3-5% partial melt bands and 20% sheets mafic and intermediate schist (MS 7). Amphibolite schist is equigranular with needles of amphibole.	main lithology	diatexite	diatexite	biotite	<1%	magnetite	<1%	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Spotted; zones partial melting with porphyroblasts of biotite & magnetite replacing garnet (?); locally mylonitic.	sheet	schist	intermediate schist	-9999	-9999	-9999	-9999	-9999	-9999	grey-brown	-9999	-9999	-9999	No notes captured.	FOL - Foliation	185	72	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1048-1	whole-rock lithogeochemistry; thin section	Amphibolite schist is equigranular with needles of amphibole.	LL-23-1048-2	whole-rock lithogeochemistry; thin section	Spotted orthogneiss migmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1049	26-06-2023 12:47:33.316	59.832181	-111.019199	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Orthogneiss extends 50m along the shore. 25-35% of the outcrop is mafic and intermediate layers that are each up to 1m thick.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	-9999	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	grey	foliated	-9999	phaneritic medium (1-5mm)	No notes captured.	FOL - Foliation	350	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1050	26-06-2023 13:02:17.001	59.832963	-111.013982	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	0.4	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mylonitic orthogneiss with 30% mafic layers. MS 0.4.	main lithology	mylonite	mesomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	Porphyroclasts; local partial melting evidence.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	182	85	-9999	-9999	SH - Shear Ductile	40	80	-9999	Migmatite in shears.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1051	26-06-2023 13:23:33.043	59.820688	-111.006785	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Huge outcrop area. There are some zones of pink granite without porphyroclasts that are probably a later intrusive phase. No mafic xenoliths or layers are present here.	main lithology	mylonite	protomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	-9999	porphyritic	phaneritic coarse (5-10mm)	Porphyroclasts; no mafic layers.	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	white-pink	foliated	-9999	phaneritic medium (1-5mm)	No Porphyroclasts	FOL - Foliation	150	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1051-1	whole-rock lithogeochemistry	Granite mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1052	26-06-2023 14:00:53.477	59.818931	-111.011873	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Approximately 80% of the outcrop is felsic medium grained granitic orthogneiss. 20% is mafic to intermediate layers and xenoliths.	main lithology	gneiss	orthogneiss	biotite	5-10%	chlorite	1-5%	-9999	-9999	white to pink	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	dark grey	-9999	-9999	phaneritic fine (0.5-1mm)	No notes captured.	FOL - Foliation	175	68	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1052-1	whole-rock lithogeochemistry; thin section	Amphibolite.	LL-23-1052-2	whole-rock lithogeochemistry	Orthogneiss, felsic medium grained granitic ogn.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1053	26-06-2023 14:31:06.148	59.837880	-111.030350	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	0.3	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Orthogneiss with biotite rich xenoliths. The xenoliths appear to be 50% biotite. There are also 1m wide amphibolite layers with epidote and kspar alteration. Measurements - MS 0.3.	main lithology	gneiss	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	amphibolite	epidote	<1%	-9999	-9999	-9999	-9999	-9999	foliated	-9999	phaneritic fine (0.5-1mm)	No notes captured.	FOL - Foliation	210	73	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1053-1	whole-rock lithogeochemistry	Amphibolite.	LL-23-1053-2	whole-rock lithogeochemistry	Quartz vein breccia from lake.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1054	26-06-2023 15:08:42.481	59.834572	-111.033237	Internal GPS	Courtney Reimert	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Change in rock type as you go up outcrop; lakeshore is spotted migmatite with 2% biotite and lots of biotite rich xenoliths. Sketch in notebook. There is a flood of quartz veining and pegmatitic pods up the hill.	main lithology	gneiss	orthogneiss	garnet	<1%	chlorite	<1%	epidote	<1%	pink	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	minor lithology	granitoid	quartz-rich granitoid	-9999	-9999	-9999	-9999	-9999	-9999	hematite pink	-9999	-9999	pegmatitic	Looks like quartz flooding.	FOL - Foliation	191	72	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1054-1	whole-rock lithogeochemistry	Quartz-rich granitoid - looks like quartz flooding.	LL-23-1054-2	whole-rock lithogeochemistry; thin section	Lower orthogneiss/migmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1055	26-06-2023 16:08:01.249	59.827849	-111.030071	Internal GPS	Courtney Reimert	Russell Hartlaub	0.56	-9999	4	-9999	-9999	-9999	-9999	-9999	-9999	Approximately 35% of the outcrop is amphibolite sheets up to 2m thick. The sheets are commonly boudinaged and have a MS of 4.0. 65% of the OC is a white to pale yellow coarse grained quartzofeldspathic gneiss with MS of 0.56.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	amphibolite	magnetite	<1%	-9999	-9999	-9999	-9999	grey	foliated	-9999	phaneritic fine (0.5-1mm)	Up to 2m wide, slightly magnetic.	FOL - Foliation	179	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1055-1	whole-rock lithogeochemistry; thin section	Amphibolite.	LL-23-1055-2	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1056	28-06-2023 09:13:13.496	59.866133	-111.018738	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Lakeside; trace graphite in the paragneiss. Third sample taken of paragneiss. Take thin section of all 3 samples. Heterogeneous brown well layered gneissic rock. 30% of outcrop is pegmatitic melt sheets.	main lithology	gneiss	paragneiss	garnet	1-5%	sillimanite	<1%	-9999	-9999	-9999	-9999	-9999	-9999	Garnet appears to be retorgressed.	minor lithology	granitoid	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	Melt sheets.	FOL - Foliation	48	78	-9999	-9999	STR - Glacial stria	45	-9999	-9999	These obvious stria may not be glacial- may be lakeshore ice stria. Variable 041-048.	-9999	-9999	-9999	-9999	-9999	LL-23-1056-1	whole-rock lithogeochemistry; thin section	Paragneiss with trace graphite.	LL-23-1056-2	whole-rock lithogeochemistry; thin section	Several pieces of paragneiss.	LL-23-1056-3	whole-rock lithogeochemistry; thin section	Pelite (paragneiss) contains graphite and possibly retrogressed garnet.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1057	28-06-2023 09:44:32.825	59.865879	-111.018600	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.035	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pegmatite. Late stage shear veins. Measurements - MS 0.035.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink to grey	-9999	-9999	pegmatitic	Quartz flooding.	minor lithology	gneiss	paragneiss	garnet	5-10%	sillimanite	<1%	-9999	-9999	banded grey-buff	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1057-1	whole-rock lithogeochemistry	Pegmatitic melt sheet.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1058	28-06-2023 10:25:50.006	59.866853	-111.010376	Internal GPS	Alex MacNeil	Russell Hartlaub	0.05	-9999	0.6	-9999	-9999	-9999	-9999	-9999	-9999	Small island.  Biotite rich sheets (schist) with MS 0.6 as well as amphibolite. Granitic component has an MS of 0.05. There is some late epidote and potassic alteration.	main lithology	gneiss	orthogneiss	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	341	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1058-1	whole-rock lithogeochemistry; thin section	Biotite rich schist/sheet.	LL-23-1058-2	whole-rock lithogeochemistry; thin section	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1059	28-06-2023 10:57:12.450	59.870756	-111.006758	Internal GPS	Alex MacNeil	Russell Hartlaub	0.35	-9999	22	-9999	-9999	-9999	-9999	-9999	-9999	Pyroxene rich parts with high mag susceptibility. These mafic pods are boudinaged and rounded.  Measurements - MS 0.35 (the regular orthogneiss); MS 22 (pyroxene rich parts).	main lithology	gneiss	orthogneiss	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	phaneritic coarse (5-10mm)	No notes captured.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	355	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1059-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1060	28-06-2023 11:19:48.391	59.872480	-110.999856	Internal GPS	Alex MacNeil	Russell Hartlaub	0.65	-9999	12	-9999	-9999	-9999	-9999	-9999	-9999	Huge outcrop area 100m by 100m. MS 0.65-12. Quite variable.	main lithology	mylonite	protomylonite	biotite	5-10%	chlorite	<1%	-9999	-9999	-9999	-9999	-9999	-9999	Coarse Grained Arch Lake type megacrystic proto-mylonite. Quartz is 30% but heavily ribboned.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	345	77	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1060-1	whole-rock lithogeochemistry	Coarse grained megacrystic protomylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1069	29-06-2023 10:22:53.981	59.789391	-111.067149	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.45	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Obvious geological contact between one unit and richly garnetiferous unit with irregular thick white contorted quartz veins (MS 0.45).  Large clots of magnetite locally in non-garnet unit, with and without qtz decimetre scale veins and eyes.	main lithology	gneiss	paragneiss	garnet	20-50%	biotite	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	minor lithology	mafic rocks	mafic schist	magnetite	1-5%	tremolite	10-20%	-9999	-9999	-9999	-9999	-9999	phaneritic medium (1-5mm)	No notes captured.	FOL - Foliation	215	70	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1069-1	whole-rock lithogeochemistry	Quartz vein chunks.	LL-23-1069-2	whole-rock lithogeochemistry; thin section	Mafic schist with magnetite-tremolite assemblage.	LL-23-1069-3	whole-rock lithogeochemistry; thin section	Garnet rich mafic or intermediate schist.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1070	29-06-2023 11:16:05.201	59.789902	-111.068922	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pegmatite unit in unit that differs from 1069. Significant lichen cover.	main lithology	metatexite	granite	magnetite	1-5%	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Granite migmatite.	sill	gabbroid	pegmatite sill	-9999	-9999	-9999	-9999	-9999	-9999	dark pink	-9999	-9999	-9999	No notes captured.	FOL - Foliation	220	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1070-1	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1071	29-06-2023 11:51:04.806	59.791111	-111.072863	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Halo. Decimetre scale clots of garnet. Intruding granite pegmatites.	main lithology	diatexite	paragneiss	garnet	10-20%	sillimanite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	garnet	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	Granite pegmatite with garnet.	FOL - Foliation	210	81	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1071-1	whole-rock lithogeochemistry; thin section	Garnet and sillimanite rich paragneiss to migmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1072	29-06-2023 13:05:00.313	59.790447	-111.072764	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quick station for pegmatite, difficult to sample.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1072-1	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1073	29-06-2023 13:27:31.328	59.788863	-111.068885	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	26	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Good compositional layering in this garnet paragneiss to migmatite. 10% pegmatitic melt pods. MS - 26.	main lithology	gneiss	paragneiss	garnet	10-20%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	No notes captured.	FOL - Foliation	217	69	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1074	29-06-2023 14:14:21.138	59.775082	-111.060134	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.8	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Short traverse. K-spar megacrystic. Arch Lake Granitoid. No mafic layers or xenoliths. grades into protomylonite. Measurements - MS 0.8.	main lithology	granitoid	granite	biotite	5-10%	chlorite	1-5%	epidote	<1%	-9999	-9999	porphyritic	phaneritic coarse (5-10mm)	Pink and white with local vibrant hematite staining/trace hematite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	255	73	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1075	29-06-2023 14:54:19.735	59.775004	-111.055289	Internal GPS	Alex MacNeil	Russell Hartlaub	2	-9999	3	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous outcrop. 45% K-spar phenocrysts. Measurements - MS 2 to 3.	main lithology	granitoid	granite	biotite	1-5%	chlorite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1075-1	whole-rock lithogeochemistry	Granite with 45% kspar phenocrysts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1076	29-06-2023 15:20:04.956	59.773718	-111.051746	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Small scale fault in outcrop. Megacrystic with interesting lineation fabric. Arch lake granite type. Lots of nice clean outcrop here.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1077	29-06-2023 15:42:57.706	59.775449	-111.054344	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strong hematite staining and parallel joint sets. Halo utilized. Same as previous.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	VN - Vein	290	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1078	30-06-2023 08:39:03.630	59.715316	-111.266318	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.01	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Shore of McLelland Lake, dropped off by float plane for traverse. Beautiful outcrop with white weathering leucocratic granite with abundant quartz veining. Mag susc is very low. There are some small faults that look like they locally have pseudotachylite. Measurements - MS 0.01.	main lithology	granitoid	granite	biotite	5-10%	-9999	-9999	-9999	-9999	off white	-9999	equigranular	phaneritic coarse (5-10mm)	Prominent quartz veining with box work development. There is some finer grained zones, but predominantly coarse grained.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	VN - Vein	320	86	-9999	-9999	LINM - Lineation mineral	220	49	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1078-1	whole-rock lithogeochemistry; thin section	Leucocratic granite with abundant quartz veining.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1079	30-06-2023 09:47:52.174	59.714322	-111.264823	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Impressive pegmatite with feldspar crystals up to 15 cm. There is some brittle faulting here. Numerous sub-parallel zones of quartz veining almost stockwork just 50m east of outcrop.	main lithology	granitoid	granite	biotite	5-10%	garnet	<1%	-9999	-9999	buff	-9999	-9999	pegmatitic	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LINM - Lineation mineral	195	40	-9999	-9999	FT - Fault Brittle	350	84	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1079-1	whole-rock lithogeochemistry	Quartz vein possible fine disseminated sulphides.	LL-23-1079-2	whole-rock lithogeochemistry; thin section	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1080	30-06-2023 10:22:43.637	59.714271	-111.262864	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz stockwork. Quartz veining makes up 40% of the outcrop. Granite is very leucocratic here.  Measurements - MS 0.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	vein	-9999	-9999	quartz	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	VN - Vein	145	70	-9999	Stockwork.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1081	30-06-2023 10:40:27.111	59.714744	-111.261439	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	The granite here is injected by 20% later pegmatitic granite. 10% of the outcrop has hematitic staining.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	dike	granitoid	dike	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	Pegmatite.	VN - Vein	160	40	-9999	Pegmatite dike orientation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1081-1	whole-rock lithogeochemistry	Pegmatite cross-cutting granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1082	30-06-2023 11:14:40.517	59.714548	-111.257479	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.01	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Locally hematitic zones and pegmatitic patches. Some areas have trace garnet, but this is only in the quartz rich pegmatitic patches. MS 0.01.	main lithology	granitoid	granite	garnet	<1%	biotite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	Local hematite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FT - Fault Brittle	180	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1082-1A	whole-rock lithogeochemistry	Granite with purple quartz.	LL-23-1082-1B	whole-rock lithogeochemistry	Granite with purple quartz.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1083	30-06-2023 11:43:02.866	59.713839	-111.255154	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Garnet patches. Purple quartz in the pegmatitic patches, Granite is coarse grained here.	main lithology	granitoid	granite	garnet	<1%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Composition - 30% quartz, 40% k-spar, 25% plag, 5% biotite and trace garnet. Garnets are up to 5cm.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1083-1	whole-rock lithogeochemistry	Granite with purple quartz.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1084	30-06-2023 12:11:32.281	59.712686	-111.251755	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Significant lichen cover. There is a significant quartz vein here that is up to 1.5 m wide here and extends to the next outcrop.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	VN - Vein	110	77	-9999	Significant quartz vein at least 40 cm and locally 1 m wide. White.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1084-1	whole-rock lithogeochemistry	Quartz vein, up to 1.5 m wide and extending to LL-23-1085-1.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1085	30-06-2023 18:08:54.805	59.712103	-111.249844	Manual Entry	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	The quartz vein from the previous outcrop extends to here. No visible economic mineralization. up to 2.5m wide here.	vein	-9999	-9999	quartz	>50%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz vein continued all the way from previous outcrop. Old, white, highly strained component of orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1086	30-06-2023 13:17:35.694	59.711424	-111.248682	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Slave granite with injected pegmatite.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	garnet	<1%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	pegmatitic	No notes captured.	FOL - Foliation	65	50	-9999	-9999	LINM - Lineation mineral	155	40	-9999	-9999	VN - Vein	75	86	-9999	-9999	LL-23-1086-1	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1087	30-06-2023 13:37:43.857	59.710797	-111.247330	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strong foliation - quick station. The granite is sheared here along the edge of a valley. 10% quartz veins here. Mylonite only extends about 20 m in the valley.	main lithology	mylonite	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Ribboned.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	280	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1088	30-06-2023 13:51:13.484	59.709536	-111.246420	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	White, buff coarse grained granite.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	75	68	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1088-1	whole-rock lithogeochemistry	Pegmatite with significant quartz content.	LL-23-1088-2	whole-rock lithogeochemistry	Foliated granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1089	30-06-2023 14:24:57.383	59.708115	-111.244714	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Granite is lineated here. Moderately foliated. Coarse grained.	main lithology	granitoid	granite	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	51	46	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1090	30-06-2023 14:48:01.652	59.706851	-111.242009	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pink, strongly foliated and folded granite with a good lineation plunging south.	main lithology	granitoid	granite	garnet	<1%	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LINF - Lineation fold	160	59	-9999	Open.	LINM - Lineation mineral	190	40	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1091	30-06-2023 15:09:50.695	59.705581	-111.241931	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strong mineral lineation here that is plunging to the south. Not as much pegmatite in this area.	main lithology	granitoid	granite	garnet	<1%	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	Coarse grained.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LINM - Lineation mineral	180	45	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1091-1	whole-rock lithogeochemistry; thin section	Granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1092	30-06-2023 15:35:43.561	59.703841	-111.243002	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same as previous.	main lithology	granitoid	granite	biotite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	70	79	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1093	30-06-2023 15:51:47.206	59.702520	-111.242625	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Heavy lichen cover but can see strong foliation. Granite is pink and coarse grained.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	58	58	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1095	01-07-2023 09:34:32.124	59.896028	-111.000026	Internal GPS	Levi Knapp	Russell Hartlaub	0.14	-9999	0.8	-9999	-9999	-9999	-9999	-9999	-9999	There is no station 1094. This is an island in the lake. 25% of the outcrop is amphibolite gneiss with strung out banding. Small porphyroclasts are visible. Measurements - MS 0.14 (in orthogneiss); MS 0.8 (in amphibolite).	main lithology	mylonite	orthogneiss	chlorite	1-5%	biotite	1-5%	-9999	-9999	-9999	-9999	-9999	phaneritic medium (1-5mm)	Porphyroclasts up to 5mm in a couple zones.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	345	81	-9999	-9999	LINF - Lineation fold	230	20	-9999	Close.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1096	01-07-2023 10:04:55.978	59.898559	-110.989482	Internal GPS	Levi Knapp	Russell Hartlaub	-9999	2.4	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Porphyroclastic Arch Lake Granite. Pink and hematitic in places. No mafic layers or xenoliths. Very homogeneous. Measurements - MS 2.4.	main lithology	mylonite	protomylonite	chlorite	5-10%	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Porphyroclasts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	10	72	-9999	-9999	LINF - Lineation fold	210	78	-9999	Open.	-9999	-9999	-9999	-9999	-9999	LL-23-1096-1	whole-rock lithogeochemistry; thin section	Mylonitic porphyroclastic Arch Lake granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1097	01-07-2023 11:10:47	59.885147	-111.011605	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Migmatitic paragneiss. Looks like sillimanite and cordierite are present.	main lithology	gneiss	paragneiss	garnet	5-10%	biotite	10-20%	sillimanite	1-5%	brown grey	gneissic	migmatitic	phaneritic coarse (5-10mm)	Good compositional layering.	sheet	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	foliated	equigranular	phaneritic coarse (5-10mm)	Leucogranite layer parallel.	FOL2 - Foliation gen2	138	85	Foliation moderate	Defined by garnet and sillimanite.	FOL1 - Foliation gen1	348	82	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1098	01-07-2023 11:58:36.782	59.909166	-111.006165	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Very mixed mylonite. Porphyroclastic. banded with green brown paragneiss. It looks like the Arch Lake granite is injected into the paragneiss and then sheared.	main lithology	mylonite	mesomylonite	chlorite	1-5%	garnet	1-5%	biotite	10-20%	green brown alternations	-9999	-9999	-9999	Ribboned.	minor lithology	mylonite	protomylonite	biotite	10-20%	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Granite and porphyroclasts.	FOL1 - Foliation gen1	160	76	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1099	01-07-2023 13:11:03.373	59.916178	-110.999341	Internal GPS	Alex MacNeil	Russell Hartlaub	-9999	0.2	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Amphibolite lenses in the orthogneiss mylonite. MS 0.2.	main lithology	mylonite	orthogneiss	chlorite	1-5%	biotite	1-5%	-9999	-9999	-9999	-9999	-9999	-9999	Hematized. High cps.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	10	86	-9999	-9999	FT - Fault Brittle	280	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1100	01-07-2023 15:02:47.078	59.809110	-111.032491	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Camp location, this is our classic orthogneiss package. However, it’s likely that this is a volcanic package that may include volcaniclastic and clastic (low aluminum) sediments. There is some evidence of compositional layering.	main lithology	gneiss	orthogneiss	biotite	5-10%	chlorite	<1%	-9999	-9999	buff	gneissic	migmatitic	phaneritic medium (1-5mm)	Partial melt seems to be apparent.	sheet	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	black	gneissic	-9999	phaneritic coarse (5-10mm)	Sheets and layers of various thicknesses (1cm to 1m).  Also some biotitic layers.	FOL1 - Foliation gen1	200	60	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1101	02-07-2023 10:49:32.737	59.808283	-111.051776	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	0.02	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Spotted migmatite and a mafic orthogneiss. Coarser grained than at camp (1100) with pegmatitic melt patches. Up the hill we see biotite rich schist that looks like paragneiss. Measurements - MS 0.02.	main lithology	gneiss	orthogneiss	biotite	10-20%	chlorite	5-10%	hypersthene	<1%	dark pink	gneissic	migmatitic	phaneritic very coarse (10-50mm)	Coarser and more magic than camp, 20% mafic and biotitic schlieren and layers, hypersthene?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	190	80	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1101-1	whole-rock lithogeochemistry	Mafic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1102	02-07-2023 11:27:18.904	59.808054	-111.052648	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	1300	-9999	-9999	-9999	Vein/layer with brilliant green copper or nickel in quartz. Fuchsite? Measurements - Scint max 1300 cps along strike.	vein	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	brilliant green	-9999	-9999	-9999	Fuchsite?	main lithology	mafic rocks	para-amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	black and rusty brown	layered	migmatitic	phaneritic medium (1-5mm)	Horizon of layered rusty mafic rocks (10 m thick).	FOL1 - Foliation gen1	200	78	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1102-1	whole-rock lithogeochemistry	Quartz vein, assay for precious metals.	LL-23-1102-2	whole-rock lithogeochemistry; thin section	Amphibolite layered. Mafic component.	LL-23-1102-3	whole-rock lithogeochemistry; thin section	Channel saw extraction of fuchsitic quartz vein.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-1103	02-07-2023 12:25:03.326	59.807877	-111.053080	Internal GPS	Russell Hartlaub	Russell Hartlaub	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Near old mineral occurrences. Gossanous zone at top of hill.	main lithology	mafic rocks	para-amphibolite	feldspar	-9999	-9999	-9999	-9999	-9999	black and grey	layered	migmatitic	phaneritic medium (1-5mm)	Layered mafic with a gossanous quartz vein at the west side. Paragneiss on the west of the vein (contact).	vein	-9999	-9999	-9999	-9999	quartz	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-1103-1	whole-rock lithogeochemistry	Quartz vein from top of hill, contains sulphides.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2001	23-06-2023 09:04:26.393	59.809628	-111.050964	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartzofeldspathic gneiss with abundant cm- to m-scale mafic enclaves strung out along the shear trend. Local m-scale injections of alkali feldspar granite, similar to what we saw intruding the Rutledge River complex at LL-23-1001; abundant qtz ribbons and stringers; mylonitic.	main lithology	gneiss	orthogneiss	biotite	10-20%	alkali-feldspar	20-50%	plagioclase	5-10%	grey	mylonitic	equigranular	phaneritic medium (1-5mm)	Approx 25% kfsp. Heavily altered biotite. Possibly some hornblende. 20-25%qtz. Interesting yellowish alteration. Locally mylonitic. Biotite granite gneiss. Local meter scale injections of alkali granite.	enclave	mafic rocks	-9999	biotite	20-50%	plagioclase	5-10%	hornblende	5-10%	dark grey to black	schistose	equigranular	phaneritic fine (0.5-1mm)	Mafic enclave. Couldn’t sample. Biotite looks to be retrograding from hornblende. Qtz biotite plag hornblende. Very magnetic, with chloritic overprint. Possible magnetite porphyry.	FOL1 - Foliation gen1	15	84	Foliation strong	Fol1 anastomosing.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2001-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2002	23-06-2023 10:37:33.193	59.810809	-111.053926	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mini station; increased biotite content, abundant foliation parallel quartz veins up to 0.3m wide. Moving west, main lith becomes increasingly migmatitic and kspar-rich; also increase in grain size.	main lithology	diatexite	diatexite	biotite	20-50%	plagioclase	10-20%	hypersthene	5-10%	grey	migmatitic	equigranular	phaneritic medium (1-5mm)	Hypersthene? More abundant than prev station. Less kfsp than prev stn. More plag and qtz. Silvery metallic mineral. Still seeing mafic enclaves and cross cutting alkali granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	30	89	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2002-1	whole-rock lithogeochemistry	Migmatitic orthogneiss with potential hypersthene.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2003	23-06-2023 11:11:17.762	59.811508	-111.059211	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Increasing kfsp and crystal size away from shear zone.  M-scale pegmatite interlayered with large pods of laminated mafic amphibolites with discordant internal foliation.	main lithology	mafic rocks	para-amphibolite	hornblende	10-20%	plagioclase	10-20%	chlorite	20-50%	greenish grey	migmatitic	porphyritic	phaneritic very fine (0.1-0.5mm)	Strongly magnetic (magnetite?). Very fine grained hornblende probably retrograding to biotite and chlorite. Green is chlorite? Pyroxene? Scratches easily though so maybe hornblende and biotite altering to chlorite. Local leucosome along contact with pegmatite.	sheet	metatexite	granite	alkali-feldspar	20-50%	quartz	10-20%	plagioclase	5-10%	buff	-9999	equigranular	pegmatitic	Leucosomal pegmatite. Cuts main unit and slightly oblique.  Biotite in pegmatite.	FOL1 - Foliation gen1	14	89	Foliation moderate	Mafic Lith 1.	IGC - Contacts	28	90	-9999	Pegmatite contact with mafic.	-9999	-9999	-9999	-9999	-9999	LL-23-2003-1	whole-rock lithogeochemistry; thin section	Strongly magnetic amphibolite.	LL-23-2003-2	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2004	23-06-2023 12:39:59.211	59.811641	-111.059621	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Very green mineral stopped us; appears to be a high strain, mylonitized migmatite of paragneiss parentage; mm- to -cm-scale compositional layers locally comprise smeared out, recrystallized garnet and record dextral asymmetric folding.	main lithology	gneiss	paragneiss	alkali-feldspar	20-50%	garnet	1-5%	epidote	20-50%	grey	mylonitic	-9999	-9999	Composition - 30% kfsp, 10-20% qtz. Hypersthene? hornblende retrograding to biotite. Unsure if green mineral is epidote. Maybe actinolite/hornblende. More mafic layers a bit more magnetic. Iridescence observed — possible labradorite (10-20%).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	0	90	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2004-1	whole-rock lithogeochemistry	Mylonitized migmatite of paragneiss parentage - interesting green minerals.	LL-23-2004-2	whole-rock lithogeochemistry; thin section	Mylonitized migmatite of paragneiss parentage - interesting green minerals.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2005	23-06-2023 13:47:25.699	59.813944	-111.064012	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Higher plagioclase content than previous unit; into Slave granite; locally, and perpendicular to strike, there is variation is the concentrations of K-spar vs. Plag; generally 20-25% Kspar and 10-20% plag; quartz (~20%).	main lithology	granitoid	granite	biotite	10-20%	chlorite	1-5%	plagioclase	10-20%	white	foliated	porphyritic	phaneritic coarse (5-10mm)	Foliated orthogneiss, with 20-25% kfsp, 10-20% plag, 30-35% qtz, 20% biotite. Hornblende retrograding to biotite. Could call this a foliated granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	15	90	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2005-1	whole-rock lithogeochemistry; thin section	Foliated granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2006	23-06-2023 14:42:42.685	59.814278	-111.069236	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Green porphyoblasts of chlorite/ chloritoid (?) abundant mm-wide, cm-long porphyroblastic stringers of epidote (?) pistachio green, strung out parallel to Strain= 020/90.	main lithology	granitoid	granite	alkali-feldspar	10-20%	quartz	20-50%	biotite	20-50%	white	foliated	porphyritic	phaneritic medium (1-5mm)	Qtz 35%, kfsp 10-20, plag 10-20, retrograde biotite from hornblende, green porphyoblasts (stringers parallel to foliation. Pistachio green. Epidote?).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	20	82	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2006-1	whole-rock lithogeochemistry	Granite with green phorphyroblasts.	LL-23-2006-2	whole-rock lithogeochemistry; thin section	Granite with green phorphyroblasts.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2007	23-06-2023 15:42:03.830	59.815324	-111.071517	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	biotite	20-50%	alkali-feldspar	20-50%	epidote	10-20%	white	foliated	porphyritic	phaneritic coarse (5-10mm)	Kfsp 20%. Qtz 30-40%. Plag 10-20%,. Biotite 20-25%. Green mineral 20-25% (epidote/tremolite/chlorite? Same as prev station). Biotite prob from hornblende, and porphyoblastic and strung out and mm scale. Orthogneiss granite. In some area porphyoblasts are darker and are biotite but in some areas are lighter and associated with mm scale hornblende needles.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	24	90	Foliation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2007-1	whole-rock lithogeochemistry	Granite with green phorphyroblasts.	LL-23-2007-2	whole-rock lithogeochemistry; thin section	Granite with green phorphyroblasts.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2008	24-06-2023 08:57:40.923	59.800765	-111.010471	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	First station of day 2. Confirm location of 2008, 2009, 2010 with GPS.	main lithology	gneiss	orthogneiss	biotite	20-50%	feldspar	20-50%	quartz	20-50%	white	gneissic	equigranular	-9999	Felsic component: Medium grained, quartzofeldspathic granite gneiss. Up to 25% feldspar, difficult to distinguish kfsp from plag. 20-50% qtz. Feldspar phenocrysts mm scale. Significant hematite staining. Possible cordierite. Mafic layers composed of extremely fg biotite and chlorite, very magnetic. Mm scale black phenocrysts. Possible presence of labradorite. Plag present. Green tint. Possible hornblende. Potentially migmatitic, with the paleo some being the felsic component, 30-40% neosome made of quartz leucosome, in situ, and 30 percent melanosome (mafic component).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	184	90	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2008-1	whole-rock lithogeochemistry	Orthogneiss felsic component.	LL-23-2008-2	whole-rock lithogeochemistry	Orthogneiss mafic component.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2009	24-06-2023 09:44:22.169	59.801251	-111.018065	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same unit, less strain, m-scale felsic and mafic component interlayered; mafic layers may represent lenses of gabbroic amphibolite, interlayered with a younger melt granite and are cut by cm-scale, foliation parallel quartz leucosome.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2010	24-06-2023 10:07:48.164	59.802318	-111.016354	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Strikingly green enclaves of gabbroic amphibolite(?) separating felsic and mafic components into separate lithologies; possibly 3 components (an older, orthogneiss intruded and foliated with younger melt granite, and with the presence of mafic enclaves/schlieren). Pervasive isoclinal folding best displayed by leucosome. Sinistral riedel shears and S-folds commonly observed. Both lithologies magnetic, mafic lith more strongly. Meter scale layering.	main lithology	gneiss	granite	feldspar	20-50%	hornblende	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	Plag and kfsp present. Contains abundant insitu leucosome.	enclave	gabbroid	amphibolite	biotite	20-50%	hornblende	20-50%	-9999	-9999	-9999	-9999	-9999	-9999	Mafic component. Melanosome. Graphite? Hornblende is massive or amorphous.	FOL - Foliation	183	89	Foliation strong	76->195: plunge and trend.	AXF - Axial fold plane	185	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2010-1	whole-rock lithogeochemistry; thin section	Orthogneiss felsic component.	LL-23-2010-2	whole-rock lithogeochemistry; thin section	Amphibolite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2011	24-06-2023 10:51:56.788	59.800983	-111.012792	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Did not pass through Slave granite; rather, this rock resembles a potential transitional contact into the Arch Lake granite. Decametre to meter scale layering of more resistant Felsic layers with more biotite rich mafic layers which are more weathered, and may represent mafic component of western orthogneiss. Protomylonitic ribbons of qtz and fsp; overall, its a protomylonitic granitoid of predominantly quartzofeldspathic, buff weathering, attenuated and boudinaged layers (forming cm-scale porphyroclasts).	main lithology	granitoid	protomylonite	alkali-feldspar	20-50%	quartz	20-50%	-9999	-9999	-9999	-9999	-9999	-9999	Feldspar megacrysts. (max 2x3cm) Quartz ribbons. Codierite/blue quartz. Matrix is extremely fine grained and mafic: predominantly biotite and hornblende. 60% matrix, 40% kfsp and qtz/cordierite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	15	86	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2011-1	whole-rock lithogeochemistry	Protomylonitic granitoid, predominantly quartzofeldspathic.	LL-23-2011-2	whole-rock lithogeochemistry	Protomylonitic granitoid, predominantly quartzofeldspathic.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2012	24-06-2023 11:36:49.438	59.801520	-111.009530	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Comprises pink and grey gneiss; pink quartzofeldspathic, fine to med. grained quartz and feldspar, with plagioclase phenocrysts (white to grey weathering up to multiple cm's in size) and generally angular. Unable to identify any aluminous minerals; possible cordierite, but may be blue quartz. Roughly 10-20% plag, 20-50% kspar, in bands. The grey component: mafic, very magnetic, and spotted with microcrystalline, equant red minerals (garnet?) amidst plagioclase, hornblende, biotite (retrograde) and possible pyroxene.	main lithology	granitoid	mylonite	alkali-feldspar	20-50%	plagioclase	20-50%	biotite	10-20%	-9999	gneissic	porphyritic	phaneritic very coarse (10-50mm)	About 20% matrix, 80% plag and qtz. Fresh surface is extremely waxy. 30-40% kfsp. Possible cordierite. Phaneritic c to vc; Day and station cut short due to extreme weather conditions.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	197	90	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2012-1	whole-rock lithogeochemistry	Mylonitic gneiss/granitoid material similar to previous station, predominantly quartzofeldspathic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2013	24-06-2023 12:55:02.063	59.801410	-111.018821	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Back in vicinity of station LL-23-2008. Seeing boudinaged white weathering orthogneiss, with enclaves and interlayers of 10cm- wide coarse-grained amphibolite. Local patches of younger melt granite are coarse grained to pegmatitic and interlayered; possibly injected, this younger material is boudinaged with the foliation; 5-10% biotite porphyroblasts, well-foliated.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	195	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2013-1	whole-rock lithogeochemistry	Amphibolite enclave.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2014	25-06-2023 10:03:44.768	59.927187	-111.003220	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Rusty gossanous mafic amphibolite along shoreline. Gneissic fabric (red and black bands). Mylonitic orthogneiss.	main lithology	gneiss	orthogneiss	biotite	20-50%	plagioclase	20-50%	hornblende	20-50%	reddish brown to black weathering	-9999	-9999	aphanitic (<0.01mm)	Extremely fine grained. Biotite, plag, probably hornblende but too fine grained to identify. Heavy hematite staining. Qtz 5-10%. Plag is heavily altered, heavily sericitized. Very very weakly magnetic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	180	83	-9999	Westward the foliation is bending clockwise relative to north.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2014-1	whole-rock lithogeochemistry	Rusty schist.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2015	25-06-2023 10:42:25.365	59.926931	-111.003701	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Layering of quartz rich leucocogranitic ribbons (mm- to dm- scale) with quartzofelspathic material of high k-spar content, with greenish-grey mafic interlayers and lenticles. Mesomylonitic with gneissic texture; foliation is bending clockwise moving west from shore.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	75	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2015-1	whole-rock lithogeochemistry	Mafic component of mylonitic orthogneiss.	LL-23-2015-2	whole-rock lithogeochemistry	Quartzofeldspathic component of mylonitic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2016	25-06-2023 11:23:26.754	59.927853	-111.004378	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same lithologies as previous unit. Mesoscopic dextral asymmetric folding is pervasive. Potentially axial planar hornblende.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	344	86	-9999	Hinge line: 75->344. Dextral limb 165/81. Sinistral limb 310/85.	FOL - Foliation	169	70	-9999	General foliation.  Oriented sample with this foliation.	-9999	-9999	-9999	-9999	-9999	LL-23-2016-1	oriented thin section	Orthogneiss, oriented sample with foliation 169/70; can check shear sense movement and correlate metamorphic minerals to structures.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2017	25-06-2023 12:52:48.053	59.929000	-111.009183	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Migmatitic and mylonitized, with anastomosing foliation. Multi-cm scale garnet orthogneiss; mm- to 5cm-scale garnets (equant to tabular), wrapped by foliation and apparently associated with leucocratic, felsic layers; being replaced by biotite and quartz matrix; garnets are concentrated in compositional layers. Mafic layers comprise hornblende, biotite and plagioclase. Injections of younger, layer parallel melt granite are abundant. On the west, unit is in contact with m- wide pegmatite, which on its western side is in contact with a transitional phase of slave granite. Garnets phasing out to the west but still present.	main lithology	gneiss	paragneiss	garnet	5-10%	biotite	20-50%	hornblende	20-50%	grey	protomylonitic	porphyritic	phaneritic medium (1-5mm)	Garnet paragneiss. Mm scale to 5cm garnet. Wrapped by mylonitic foliation and associated with leukocratic Felsic layers of qtz and feldspar. Biotite is replacing garnet.	minor lithology	granitoid	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Slave granite transitional unit. Contact between Slave granite transitional unit and main Lith parallels foliation. More Felsic with leucocratic layering.	FOL - Foliation	185	89	Foliation intense	Anastomosing and intense.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2017-1	whole-rock lithogeochemistry; thin section	Garnet paragneiss from main lithology.	LL-23-2017-2	whole-rock lithogeochemistry	Slave granite transitional unit, increasingly felsic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2018	25-06-2023 13:52:21.986	59.930478	-111.012677	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Similar to last unit's main lithology; garnets (equant, mm- multi-cm-scale) leucocratic layers, wrapped by mylonitic foliation; local pods of extremely fine-grained, silty quartzitic material, enveloped by biotite, aphanitic; locally gossan near eastern shore, heavily altered and hematized.	main lithology	gneiss	paragneiss	garnet	5-10%	biotite	20-50%	hornblende	20-50%	grey	-9999	porphyritic	phaneritic medium (1-5mm)	Predominantly biotite matrix. Plag is iridescent, so maybe labradorite present. 20-50% of each of biotite, hornblende and plag. Quartz 20-30%  Contains pods of “silty” quartiztic, fine grained, light brown. Enveloped by darker layer; garnets are weathering out with perfect pentagonal crystal habit.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	165	90	-9999	Orientation highly variable across station. Measured on east side of station.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2018-1	whole-rock lithogeochemistry	Garnet paragneiss.	LL-23-2018-2	whole-rock lithogeochemistry	Heavily altered paragneiss, hematite staining.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2019	25-06-2023 14:52:18.230	59.923341	-111.018465	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Grey weathering pink and grey orthogneiss; grey quartzofeldspathic, biotite bearing older granitic component, injected layer parallel by younger, leucogranitic granite.	main lithology	gneiss	orthogneiss	biotite	20-50%	plagioclase	20-50%	quartz	10-20%	cream to grey	-9999	-9999	-9999	Gneissic. 5-10% kspar. Gold metallic mineral, think it is cubic, pyrite? Biotite seems to be retrograding from hornblende. 10-15% qtz. Abundant qtz ribbons.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	188	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2019-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2020	25-06-2023 15:29:48.451	59.922921	-111.022753	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Slave granite.	main lithology	granitoid	orthogneiss	biotite	20-50%	plagioclase	20-50%	alkali-feldspar	10-20%	white	-9999	-9999	phaneritic coarse (5-10mm)	Quartz 20%. Plag 20-25%. Biotite likely porphyroblastic, agglomerates strung out parallel to foliation. Locally the biotite porphyoblasts appear green, epidote/chlorite? Appears to resemble lithologies at station 2007. Feldspar crystals approaching 1 cm.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	185	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2020-1	whole-rock lithogeochemistry	Orthogneiss.	LL-23-2020-2	whole-rock lithogeochemistry	Garnet sillimanite migmatitic paragneiss with leucosome.	LL-23-2020-3	whole-rock lithogeochemistry	Garnet sillimanite migmatitic paragneiss; well foliated.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2021	25-06-2023 16:19:05.211	59.930752	-111.014680	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	True metasediments; not mylonitic; relatively happy/undeformed.	main lithology	gneiss	paragneiss	alkali-feldspar	20-50%	quartz	10-20%	plagioclase	20-50%	-9999	-9999	-9999	-9999	Potential cordierite. Fine grained matrix of biotite. Kfsp and plag porphyry up to 75mm grain size. Yellow alteration mineral associated with kfsp. Minor Muscovite?  Sample 2 is 10m to east. Increase in grain size fsp porphyry up to 1cm or larger. Entire rock is coarsening eastward. Clasts up to about 30cm. Feldspathic clasts with up to cm scale kfsp and plag. Feldspathic clasts envelope by mafic envelope (biotite, hornblende, plag). Quartzofeldspathic clast about 30cm also has mafic envelope and clast contains garnet(?). Clast seems to have relic garnet up to 3cm, replaced by biotite and hornblende. Mafic clast present, is folded. Size about 10cm, elongate. Isoclinal S folds observed in main lithology.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	5	75	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2021-1	whole-rock lithogeochemistry; thin section	Paragneiss.	LL-23-2021-2	whole-rock lithogeochemistry; thin section	Paragneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2022	26-06-2023 09:38:17.464	59.770200	-111.066013	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	10-20%	buff	foliated	porphyritic	phaneritic coarse (5-10mm)	Kspar megacrysts up to multiple cm across. Accessory plag. Biotite retro to chlorite and qtz bluish 10-20% Cordierite? Large, cm-scale grey to white phenocrysts of feldspar may be plagioclase.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	190	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2022-1	whole-rock lithogeochemistry	K-spar granite.	LL-23-2022-2	whole-rock lithogeochemistry; thin section	K-spar granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2023	26-06-2023 10:10:27.922	59.766457	-111.064294	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Well-foliated to protomylonitic Arch Lake granite; alternating with m-scale layers of fine- to med-grained non-megacrystic, equigranular K-spar rich granite of similar composition; melting out/being injected? Layer parallel with dominant foliation, which is verging on proto-mylonitic. 1 sample of each.	main lithology	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	10-20%	buff to light grey	foliated	porphyritic	phaneritic coarse (5-10mm)	Very nice exposure. Local deformation of qtz veins. Biotite retrograding to chlorite.	sill	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	10-20%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	190	90	Lineation moderate	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2023-1	whole-rock lithogeochemistry	Well-foliated to protomylonitic Arch Lake granite, megacrystic.	LL-23-2023-2	whole-rock lithogeochemistry; thin section	Non-megacrystic, equigranular K-spar rich granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2024	26-06-2023 10:48:07.922	59.764428	-111.061298	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Obvious cm-scale dark grey to black plag phenocrysts up to 5 cm; possible incipient replacement by k-spar (anti-perthite?). Extremely fine grained biotite matrix and qtz-plag ribbons begin to develop. Up to 30 cm wide layers of med grained granitic material with qtz veining. Similar to prev. unit; increase in grain size and abundancy of feldspar megacrysts. The dominant clast is more conclusively plagioclase rather than K-spar at this location (dark grey to black colour, 0.5 cm to 5 cm large).	main lithology	granitoid	granite	plagioclase	20-50%	alkali-feldspar	10-20%	biotite	20-50%	buff to dark grey	foliated	porphyritic	-9999	Qtz 10-15% and local deformed and contorted qtz veins; local patches of pegmatitic melt granite, generally conforming to being layer parallel with foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	20	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2024-1	whole-rock lithogeochemistry	Granite with more black plag phenocrysts.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2025	26-06-2023 11:29:52.759	59.761701	-111.055464	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No longer seeing dark-grey-black plag phenocrysts. Alteration of ground mass to chlorite? Gneissic layering of grey, quartzofeldspathic material alternating with up to 20 cm wide layers of leucogranitic qtz and kspar rich med grained buff to pink layers, which are being sheared and turned into porphyroclasts.	main lithology	granitoid	orthogneiss	alkali-feldspar	20-50%	biotite	10-20%	plagioclase	10-20%	-9999	-9999	-9999	-9999	Qtz appears bluish resembling cordierite. 20-50%; interesting shear texture (potentially sinistral shear bands?).	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	25	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2025-1	whole-rock lithogeochemistry	Gneissic k-spar granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2026	26-06-2023 11:59:39.139	59.760926	-111.053121	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Interesting outcrop, 3 samples. Third is pegmatite vein. White weathering orthogneiss alternating with mafic interlayers/enclaves; lack of megacrystic texture; quartzofeldspathic composition. Features doubly folded enclaves of mafic amphibolite (sample 2); earlier foliation parallel isoclinal folds are refolded by younger event. Why is it here? Very much resembles the orthogneiss striking through the center of Leland Lake. Cut by pegmatite dikes at an oblique angle (LL-23-2026-3).	main lithology	mylonite	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	gneissic	-9999	-9999	White and grey gneiss with folded mafic enclaves; cut by pegmatite dikes; could this be a raft of the orthogneiss caught up in Arch Lake granite?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	23	88	-9999	-9999	AXF - Axial fold plane	15	86	-9999	Fold axis 86 plunge toward 018.	-9999	-9999	-9999	-9999	-9999	LL-23-2026-1	whole-rock lithogeochemistry; thin section	Orthogneiss raft?	LL-23-2026-2	whole-rock lithogeochemistry	Mafic amphibolite enclave? Sample-oriented 013 and dip 88.	LL-23-2026-3	whole-rock lithogeochemistry	Pegmatite vein.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2027	26-06-2023 13:20:36.049	59.763210	-111.047257	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Back into Arch Lake granites for 100-200 m to west. Megacrystic feldspars clear to dark grey and weathering pink. Ribbon feldspars and quartz.	main lithology	mylonite	protomylonite	plagioclase	20-50%	alkali-feldspar	10-20%	biotite	10-20%	buff to light grey	foliated	porphyritic	phaneritic coarse (5-10mm)	Extremely fine-grained matrix of biotite retrograding from hornblende.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	43	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2027-1	whole-rock lithogeochemistry	Mylonitic granite with megacrystic feldspars.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2028	26-06-2023 13:53:48.122	59.766676	-111.040442	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz content 10-20%. Ribbons of qtz and feldspar. Small 1 cm bless of dark mafic mineral -amphibole(?) mylonitic, Arch Lake granite. Megacrystic feldspars, less abundant and smaller in size. Up to m-scale layering with buff to pink, med-fine grained Alkali feldspar granite.	main lithology	mylonite	granite	plagioclase	20-50%	alkali-feldspar	10-20%	biotite	20-50%	pink and white	foliated	-9999	-9999	Biotite retrograding from hornblende.	sill	granitoid	alkali-feldspar granite	alkali-feldspar	20-50%	plagioclase	5-10%	quartz	10-20%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	205	87	Foliation intense	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2028-1	whole-rock lithogeochemistry; thin section	Mylonitic granite with kspar.	LL-23-2028-2	whole-rock lithogeochemistry	Pink inter layered quartzose feldspathic granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2029	26-06-2023 15:00:12.213	59.766290	-111.052430	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Quartz content 15-30%. Unit contains up to 30 cm wide layers of alkali-feldspar granite; protomylonitic granite with dark grey to black porphyroclasts of plagioclase (up to 10 cm large).	main lithology	mylonite	protomylonite	plagioclase	20-50%	alkali-feldspar	10-20%	biotite	10-20%	-9999	foliated	-9999	-9999	Plag porphyroclasts up to 10 cm large.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	29	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2029-1	whole-rock lithogeochemistry	Protomylonitic granite with dark grey to black porphyroclasts of plagioclase.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2030	26-06-2023 15:38:25.837	59.764810	-111.061149	Internal GPS	Alex MacNeil	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Plag-phyric, megacrystic plagioclase with characteristic dark grey to black fresh surface color, similar mineralogy as previous units we've seen; however, the plag megacrysts appear more randomly oriented. It is verging on protomylonitic, but the foliation is weak to moderate.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	foliated	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	187	85	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2030-1	whole-rock lithogeochemistry; thin section	Plag-phyric, megacrystic plagioclase granite, verging on protomylonitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2031	28-06-2023 08:59:51.016	59.772740	-111.074050	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	biotite	20-50%	alkali-feldspar	20-50%	chlorite	20-50%	pink	gneissic	porphyritic	phaneritic medium (1-5mm)	Fine to medium grained; equigranular; biotite fine grained amorphous; retrograding from hornblende to biotite and chlorite.	dike	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	dark grey	-9999	equigranular	phaneritic fine (0.5-1mm)	No notes captured.	FOL - Foliation	46	88	-9999	-9999	IGC - Contacts	41	77	-9999	Dike; cross-cutting at low oblique angle, overprinted by main foliation.	FT - Fault Brittle	310	90	-9999	Dextral.	LL-23-2031-1	whole-rock lithogeochemistry	Mafic amphibolite dike.	LL-23-2031-2	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2032	28-06-2023 10:06:59.843	59.770254	-111.087558	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Meter scale banding of felsic and mafic components along with local leucogranite; decreased abundance of mafic xenoliths (deformed when present, with extensive quartz ribbons).  Size of banding between pink and mafic material increases to the west.	main lithology	gneiss	orthogneiss	biotite	>50%	alkali-feldspar	10-20%	plagioclase	20-50%	pink-grey	gneissic	porphyritic	phaneritic fine (0.5-1mm)	Biotite retrograding from hornblende; fine grained matrix of biotite and plag; kfsp phenoclasts; silicified.	minor lithology	granitoid	alkali-feldspar granite	alkali-feldspar	>50%	quartz	20-50%	biotite	-9999	white-light pink	-9999	-9999	phaneritic medium (1-5mm)	Leucogranite.	FOL - Foliation	226	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2032-1	whole-rock lithogeochemistry	Orthogneiss.	LL-23-2032-2	whole-rock lithogeochemistry	Leucogranite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2033	28-06-2023 11:01:29.740	59.770295	-111.095204	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Garnet paragneiss; migmatitic; garnets up to several cm in size; larger garnets tend to be concentrated on the margins of quartz leucosome.	main lithology	gneiss	paragneiss	garnet	5-10%	hornblende	20-50%	plagioclase	-9999	pink	gneissic	migmatitic	phaneritic medium (1-5mm)	Garnet irregular in shape, xenoblastic, mm to 1cm (locally up to 10cm); replaced by hornblende, biotite and plag. Leucosomal layers of cm-wide quartz, abundant garnet enveloping quartz. In-situ injection of pegmatite into the main lithology - mix of main lith and peg; silliminite (?); laths of plagioclase (?) replacing garnet (f); layers of garnet.	minor lithology	granitoid	alkali-feldspar granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	pegmatitic	Injected into main lithology.	FOL - Foliation	35	90	-9999	Protomylonitic? Intense foliation.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2033-1	whole-rock lithogeochemistry; thin section	Garnet paragneiss; would be good to identify aluminous minerals.	LL-23-2033-2	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2034	28-06-2023 11:45:33.583	59.770099	-111.096000	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	In sheared contact with previous station paragneiss to the east.  Flattened outcrop under uprooted tree at swamp level. High strain; probable intrusive granitoid.	main lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2034-1	whole-rock lithogeochemistry	Mylonitic granite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2035	28-06-2023 12:04:15.581	59.769828	-111.096767	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	mafic rocks	gabbro	plagioclase	>50%	biotite	20-50%	-9999	-9999	grey, weathered surface is white, layers of hematite staining	-9999	-9999	phaneritic medium (1-5mm)	Biotite from hornblende (?); waxy, glassy volcanic texture; up to 2cm long bundles of parallel plagioclase laths, bundles oriented randomly to each other.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	42	86	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2035-1	whole-rock lithogeochemistry	Gabbro.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2036	28-06-2023 12:42:09.803	59.769869	-111.096768	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	mylonite	ultramylonite	hornblende	20-50%	plagioclase	20-50%	-9999	-9999	dark grey and pink layers	gneissic	-9999	phaneritic very fine (0.1-0.5mm)	Mm scale laminae of pink, dark grey, light grey layers. Increasingly mylonitic to the east. So fine-grained, difficult to judge hornblende or biotite; extremely fine grained mafic matrix of 20-50% plag and 20-30% quartz and 10-20% kfsp. Local needles of hornblende. Appears pink layers (mm to 10cm) have similar mineralogy to pegmatite at NE end of outcrop.	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	pegmatitic	Vein of pegmatite (2 m) at NE edge of outcrop oblique to foliation.	FOL - Foliation	191	90	Foliation intense	Ultramylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2036-1	whole-rock lithogeochemistry; thin section	Ultramylonite.	LL-23-2036-2	whole-rock lithogeochemistry	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2037	28-06-2023 13:45:32.025	59.775953	-111.110069	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Garnet paragneiss (para amphibolite due to great amount of hornblende and plagioclase, and general mafic appearance) with probable magnetite. Intruded by m-scale dikes of alkali feldspar granite. Compositional bands of smeared out garnets alternating with qtz and feldspar. Strongly magnetic. dikes of pegmatite, as well as pegmatitic leucosome and melt patches.	main lithology	diatexite	diatexite	garnet	1-5%	biotite	20-50%	magnetite	1-5%	dark grey	foliated	-9999	phaneritic very fine (0.1-0.5mm)	Garnet xenoblastic, rarely in one piece, no larger than 1cm, nearly if not fully replaced by plag and retrograde hornblende or hornblende. Pyroxene?	dike	granitoid	alkali-feldspar granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	pink	-9999	-9999	pegmatitic	Greenish, cm-scale recessive spots may be hypersthene. Pegmatite (2-3m wide) inter layered with main lithology. On very east edge of outcrop starting to phase back into mylonite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2037-1	whole-rock lithogeochemistry; thin section	Migmatitic garnet paragneiss.	LL-23-2037-2	whole-rock lithogeochemistry; thin section	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2038	28-06-2023 14:45:26.787	59.771847	-111.098028	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Meter scale banding of granitic to pegmatite alkali feldspar granite with mafic amphibolite of potential basaltic origin.  Strike parallel but extremely anastomosed. Strong foliation in mafic units.	main lithology	diatexite	diatexite	garnet	1%	magnetite	1-5%	hypersthene	-9999	dark grey	foliated	-9999	phaneritic very fine (0.1-0.5mm)	Volcaniclastic appearance with greenish grey clasts and bands. Flow-like appearance: xenoblastic retrograde garnets; possible hypersthene; migmatitic with melt patches.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	344	90	Foliation intense	Mafic foliation. Foliation moving clockwise to the west.	FOL - Foliation	15	90	Foliation weak	Granite.	-9999	-9999	-9999	-9999	-9999	LL-23-2038-1	whole-rock lithogeochemistry	Migmatitic garnet paragneiss?	LL-23-2038-2	whole-rock lithogeochemistry; thin section	Pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2039	28-06-2023 15:10:00	59.773292	-111.093239	Manual Entry	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Ultramylonite, on strike.	main lithology	mylonite	ultramylonite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	187	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2039-1	whole-rock lithogeochemistry; thin section	Ultramylonite; could use for T.S. to verify it's sedimentary protolith.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2040	28-06-2023 15:15:00	59.773470	-111.091993	Manual Entry	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Garnet sillimanite paragneiss; migmatitic; pods of massive garnet appear associated with quartz leucosomal melting; cm-scale compositional bands of recrystallized garnet paste, folded. This grades into ultramylonite to the west. Garnets forming small, mm- to cm- scale xenoblastic crystals, in addition to amorphous, massive pods between 10 to 30 cm in size (length).	main lithology	gneiss	paragneiss	garnet	1-5%	Sillimanite	(1-5%)	-9999	-9999	light grey	gneissic	porphyritic	phaneritic medium (1-5mm)	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2040-1	whole-rock lithogeochemistry; thin section	Quartz-rich granitoid (leucosomal melting).	LL-23-2040-2	whole-rock lithogeochemistry	Garnet sillimanite paragneiss.	LL-23-2040-3	whole-rock lithogeochemistry	Garnet sillimanite paragneiss.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2041	29-06-2023 08:50:12.029	59.800435	-111.023924	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Up to 1.5 m mafic layers and xenoliths (appear as schlieren locally), pervasive isoclinal folding, layer parallel boudinage best displayed by mafic layers, partial melt zones and patches. M-scale banding of the three components of the typical orthogneiss.	main lithology	gneiss	orthogneiss	plagioclase	20-50%	quartz	20-50%	chlorite	1-5%	pink to grey	gneissic	migmatitic	phaneritic medium (1-5mm)	Alternating between white weathering older component and potentially injected and granitic, buff weathering components, and mafic enclaves/interlayers of amphibolite. Granitic component appears to be injected in situ into main orthogneiss; up to 680 cps locally within buff unit. Pegmatite biotite salvage enveloped by melanosome of biotite and chlorite. Biotite and kfsp rich in granitic component. Spotted with biotite porphyroblasts. Spots of chlorite retrograding from biotite.	minor lithology	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	grey	-9999	-9999	phaneritic fine (0.5-1mm)	Potential insitu leucosome within mafic.	FOL - Foliation	7	85	Foliation strong	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	5	83	-9999	Fold hinge: Trend 012, plunge 87 (87 toward 12).	LL-23-2041-1	whole-rock lithogeochemistry	White weathering component of orthogneiss, older.	LL-23-2041-2	whole-rock lithogeochemistry	Amphibolite, gabbro?	LL-23-2041-3	whole-rock lithogeochemistry	Also additional sample of granitic, younger component of orthogneiss.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2042	29-06-2023 09:47:29.375	59.805546	-111.031073	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Increasingly sheared, more of the granitic component here. Walked east but did not see any change into Arch Lake granite; uniform orthogneiss all the way across.	main lithology	gneiss	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	white	gneissic	migmatitic	-9999	No notes captured.	minor lithology	mafic rocks	amphibolite	epidote	-9999	-9999	-9999	-9999	-9999	grey green	-9999	-9999	-9999	Quartz epidote veining/melt in mafic layer enveloping granitic salvage. Mafic layers increasingly attenuated.	FOL - Foliation	187	88	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2043	29-06-2023 10:12:34.505	59.807359	-111.026624	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	650	-9999	-9999	-9999	Similar lithology at previous station; increased hematite staining; more mylonitic approaching shear zone to the west.	main lithology	gneiss	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	white	gneissic	migmatitic	phaneritic medium (1-5mm)	Increased amount of melt textures and in-situ leucosome compared to 2041. Increased granitic injection, decreased abundance mafic components - form 10cm layers and discontinuous layers. Up to 650 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	16	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2043-1	whole-rock lithogeochemistry; thin section	Protolith determination of mylonitic orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2044	29-06-2023 10:50:05.936	59.820728	-111.023981	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	800	-9999	-9999	-9999	Three component outcrop - orthogneiss, granitic, mafic components.  More mylonitic than previous stations.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	pink	massive	-9999	phaneritic medium (1-5mm)	Alkali granite component of orthogneiss, interlayered with primary component of orthogneiss, likely insitu melting. Granitic component becoming more coarse grained. 800 cps.	minor lithology	mafic rocks	amphibolite	biotite	>50%	plagioclase	10-20%	-9999	-9999	dark grey	massive	-9999	-9999	Sericitized plag; chlorite overprinting; possible hornblende.	FOL - Foliation	174	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2044-1	whole-rock lithogeochemistry; thin section	Mafic component of orthogneiss, amphibolite.	LL-23-2044-2	whole-rock lithogeochemistry	Coarse grained granitic component of orthogneiss - pegmatite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2045	29-06-2023 11:47:31.178	59.819901	-111.028248	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	500	3.8	21.1	3.8	Island station. Late brittle-ductile shears oriented 265; mylonitic orthogneiss; white weathering component, interlayered with highly strained, gabbroic amphibolite lenses, which display prominent quartz leucosome which is further strained along foliation. Biotite porphyroblasts.	main lithology	mylonite	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	white	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Biotite rich mafic component still present (mm to 5 cm layers, highly strained); so far all of the stations today have features biotite porphyry.	sheet	granitoid	granite	alkali-feldspar	-9999	plagioclase	-9999	biotite	5-10%	pink	migmatitic	-9999	pegmatitic	Measurements - Scint 500 cps. Assay #49 - K 3.8%, U 14.4 ppm, Th 21.1 ppm.	FOL - Foliation	3	89	-9999	-9999	FT - Fault Brittle	265	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2045-1	whole-rock lithogeochemistry	Mix of mylonitic orthogneiss, mafic layers.	LL-23-2045-2	whole-rock lithogeochemistry; thin section	Mylonitic orthogneiss, hot (assay 50 - cps??) S end of Island.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2046	29-06-2023 13:31:02.206	59.816177	-111.046328	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Gossanous 3 component orthogneiss; older, grey coloured, quartzofeldspathic gneissic component may reflect paleosome; could the mafic interlayers/enclaves represent sheared melanosome, while the buff weathering interlayers and melt patches may represent leucosome component (which tends to be radioactive).	main lithology	mylonite	orthogneiss	biotite	10-20%	-9999	-9999	-9999	-9999	white	gneissic	migmatitic	phaneritic medium (1-5mm)	Increasingly gossanous to the east; mylonitization is more pervasive in older, white weathering component and amphibolites, while the foliation is weak within the buff weathering granite injections.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	10	89	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2046-1	whole-rock lithogeochemistry	Old, white, highly strained component of orthogneiss.	LL-23-3005W	whole-rock lithogeochemistry	Dark grey, low cps mylonite on the west side of the lithological contact with red to orange orthogneiss, sampled with channel saw by Alex and Gary (hence the different sample ID).  Location is approximately 50 m northwest of Nic's LL-23-2046 station.	LL-23-3005C	whole-rock lithogeochemistry	Lithological contact between mylonite and orthogneiss, sampled with channel saw by Alex and Gary (hence the different sample ID).  Location is approximately 50 m northwest of Nic's LL-23-2046 station.	LL-23-3005E	whole-rock lithogeochemistry; thin section	Red to orange, high cps orthogneiss on the east side of the lithological contact, sampled with the channel saw by Alex and Gary (hence the different sample ID).  Location is approximately 50 m northwest of Nic's LL-23-2046 station.	Alberta Geological Survey
LL-23-2047	29-06-2023 13:56:27.462	59.816729	-111.046718	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	600	-9999	1880	1.9	271.9	1.9	Traced from shoreline to hill, 1880 cps at station point. 600-1200 cps for at least 100m down strike. Out of the gossan; alternating orthogneiss components; mineralization is restricted to buff weathering, m- wide layers. Assay #54 - Th 271.9ppm, U 2.9 ppm, K 1.9%.  	main lithology	mylonite	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	dark pink	foliated	-9999	phaneritic medium (1-5mm)	Highly strained relative to eastern outcrops earlier today. Increase in amount and intensity of hematized layers. 3m wide zones of granitic hematized anomalous zone. Does not continue up strike past station point. From station point, dead zone 7m to west then 2m zone of granite up to 1121 cps. WEST layer th 101.7 ppm, U 5.4 ppm, K 3.8 (assay 54). One sample reflects granite hot at station. 47b.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	218	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2047-1	whole-rock lithogeochemistry; thin section	Mylonitic orthogneiss, 1st thick granitic layer traced to water (1800 cps).	LL-23-2047-2	whole-rock lithogeochemistry	Mylonitic orthogneiss, 1200 cps, taken 7 m to the west of station point, at station 2047-b.	LL-23-3001	whole-rock lithogeochemistry	Granitic orthogneiss, channel sample taken by Alex and Gary (hence the different sample ID).  Location is approximately 6m southeast of Nic's LL-23-2047 station.	LL-23-3002	whole-rock lithogeochemistry	Granitic orthogneiss, channel sample taken by Alex and Gary (hence the different sample ID).  Location is on the exact location of Nic's LL-23-2047 station.	Alberta Geological Survey
LL-23-2047b	02-07-2023 08:51:46.612	59.816784	-111.046917	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	800	-9999	1900	-9999	-9999	-9999	Measurements - 800-1200cps, can trace down strike for up to ~70m, 7m west from 1900cps 2047 station.  Sample of hot thorium rich granite gneiss lumped in w station 47.  Sample 2 taken July 2 of potential metaseds in contact with granite.  Moving west, seeing more interpreting of potential metaseds, all the way until we are finally in the metaseds. Sample 3 reflects orthogneiss, not hot material with white weathering colour, inter layered in this 3 component gneiss with the sed layers and alkali feldspar granite.	main lithology	mylonite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2047b-1	whole-rock lithogeochemistry; thin section	Paragneiss unit in contact on the west with orthogneiss; should be used to ID minerals.	LL-23-2047b-2	whole-rock lithogeochemistry	White weathering, not hot component of orthogneiss inter layered with sample 1, and the lumped in sample of hot granite (2047-2).	LL-23-3003	whole-rock lithogeochemistry	Orthogneiss, channel sample taken by Alex and Gary (hence the different sample ID).  Location is approximately 20 m northeast of Nic's LL-23-2047b station.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2048	29-06-2023 14:15:07.033	59.816192	-111.047598	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	600	-9999	1200	-9999	-9999	-9999	Third layer moving from east, on strike and traced from 2047b (1200cps) ~600-1200 cps, 1m wide zone, trace down strike approx 100m. Heavily vegetated.	main lithology	mylonite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	14	86	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2049	29-06-2023 14:24:28.548	59.816894	-111.047266	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	1000	-9999	-9999	-9999	Layer of granitic material (1.5 m wide; 1000 cps), about 10 m west of previous layer, intruding and interlayered with recrystalized mylonitic presumable paragneiss. Traced approx 30 m up strike. On strike with station 2050. If not sampled, it will have been sampled by Alex (3000 series).	main lithology	mylonite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-3004	whole-rock lithogeochemistry	Orthogneiss channel sample taken by Alex and Gary (hence the different sample ID). Location is approximately 15 m north of Nic's LL-23-2049 station.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2050	29-06-2023 14:28:08.104	59.817239	-111.047055	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	1200	-9999	-9999	-9999	Layer of pink granite (1.5 m wide; 1200 cps) within recrystallized, mylonitic presumable paragneiss. Can be traced 20 m up strike.	main lithology	mylonite	paragneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	sheet	granitoid	granite	alkali-feldspar	20-50%	plagioclase	10-20%	biotite	5-10%	-9999	-9999	-9999	-9999	No notes captured.	FOL - Foliation	340	90	-9999	Contact with orthogneiss and metaseds about 20m from station.	FOL - Foliation	38	90	-9999	Foliation of main unit.	-9999	-9999	-9999	-9999	-9999	LL-23-2050-1	whole-rock lithogeochemistry	Pink granite within recrystallized, mylonitic paragneiss, 1200 cps.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2051	29-06-2023 14:31:36.087	59.817372	-111.047328	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Lithology change, contact with lower strain metasediments; which display younger folding of pre-developed S0/1/2..etc. Probable sillimanite. The interlayered granite is no longer observed moving west until the major topographic drop.	main lithology	mylonite	phyllonite	sillimanite	5-10%	-9999	-9999	-9999	-9999	grey	foliated	-9999	phaneritic fine (0.5-1mm)	Phyllonitic metasediments; extremely micaceous, sheared/folded. Thin section for mineral ID and structural/metamorphic sequencing?	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	230	90	-9999	Hinge line: trend  235 south plunging 90, axial plane: 230, 90. Second generation refolding S 1.	FOL - Foliation	140	90	-9999	Also the orientation of our Sample 1.	LINM - Lineation mineral	152	80	-9999	Plunging 80 towards 152.	LL-23-2051-1	whole-rock lithogeochemistry; oriented thin section	Phyllonitic metasediments, oriented sample.	LL-23-2051-2	whole-rock lithogeochemistry	Granite in contact with phyllonite, assuming this is barren, would be good to compare against mineralized granites.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2052	30-06-2023 09:05:31.540	59.735054	-111.218581	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Pegmatitic phase features what appears to be multi cm-scale purple quartz grains and white plagioclase grains, amidst a highly altered, white mica rich, powdery matrix. We see similar mineralogy in all pegmatites observed on this day.	main lithology	granitoid	orthogneiss	quartz	20-50%	plagioclase	20-50%	alkali-feldspar	10-20%	white to cream	foliated	-9999	pegmatitic	Granite to pegmatite, plag altering to sericite/muscovite, tonalitic? Difficult to estimate ratio of kspar and plag. Biotite rich along foliation plane., retrogressing to chlorite. Potential corderite along foliation. Yellowish alteration displayed by feldspar and biotite. Local pegmatite biotite selvage.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	350	82	Foliation weak	Very weak foliation, difficult to trace.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2052-1	whole-rock lithogeochemistry	Med-grained white granite.	LL-23-2052-2	whole-rock lithogeochemistry	Pegmatitic phase of granite, purple quartz and white plag.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2055	30-06-2023 12:46:13.579	59.733015	-111.207869	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Getting into more dominantly the finer grained granite, with the coarsest phase of pegmatite yet (feldspars up to 10 cm long).  Still have mix of medium to fine grained, with pegmatite annealing foliation planes and east west trending set of fractures/faults.  It cuts the medium grained stuff, while also coming in along foliation. Sample 1 is pegmatite, with feldspars up to 10 cm long, and 2 is the fine-grained material, that locally and on some well exposed surfaces appears leucogranitic, despite maintaining mafic minerals in matrix upon further examination.	main lithology	granitoid	granitoid	alkali-feldspar	10-20%	plagioclase	20-50%	quartz	20-50%	-9999	-9999	equigranular	phaneritic medium (1-5mm)	Medium grained component. Cut by fine grained dikes up to several meters wide, which bear chlorite porphyry of previous biotite. These appear leucogranitic and associated with pegmatite emplacement.	dike	granitoid	pegmatite dike	feldspar	>50%	quartz	20-50%	chlorite	5-10%	-9999	foliated	porphyritic	pegmatitic	Spots of chlorite, of biotite; purple quartz.	FOL1 - Foliation gen1	340	80	Foliation weak	-9999	FR - Fracture	54	90	-9999	-9999	FT - Fault Brittle	88	-9999	-9999	Pegmatite coming in along this trend, as well as the foliation.	LL-23-2055-1	whole-rock lithogeochemistry; thin section	Pegmatite.	LL-23-2055-2	whole-rock lithogeochemistry; thin section	Fine-grained aplite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2056	30-06-2023 14:28:19.691	59.731807	-111.211617	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Same stuff, took sample of all three components. 1 is pegmatite, 2 is contact of fine dike with med grained main lith of granitic comp.  Pegmatite is yellowish and chloritic, and appear more closely associated with the felsic fine grained dikes.  Locally there are patches of garnet red, however unclear if this is alteration or really deformed garnets. Contact of dike is : 020/83.	main lithology	granitoid	granitoid	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	15	90	-9999	-9999	IGC - Contacts	20	83	-9999	Contact of aplite dikes.	-9999	-9999	-9999	-9999	-9999	LL-23-2056-1	whole-rock lithogeochemistry	Pegmatite.	LL-23-2056-2	whole-rock lithogeochemistry	Contact between aplite dike and med-grained granite.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2057	01-07-2023 09:24:53.313	59.747563	-111.104237	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Orthogneiss, dominated by younger, extremely hematized biotite porphyroblastic granite. Local and rare mafic enclaves.	main lithology	gneiss	orthogneiss	biotite	>50%	quartz	-9999	alkali-feldspar	20-50%	buff grey	gneissic	-9999	phaneritic medium (1-5mm)	Hornblende-biotite retrograde layers alternating with bands of quartz and kfsp. Possible cordierite.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	224	90	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2057-1M	whole-rock lithogeochemistry	Orthogneiss. Sample listed as "massive", same material as LL-23-2057F.	LL-23-2057-1F	whole-rock lithogeochemistry	Orthogneiss. Sample listed as "foliated", same material as LL-23-2057-1M.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2058	01-07-2023 09:42:06.504	59.748374	-111.102115	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	North end of island; only seeing pink weathering biotite granite gneiss component, reflecting the high topography of the island. Sample 2 reflects mafic enclave.	main lithology	gneiss	orthogneiss	biotite	-9999	-9999	-9999	-9999	-9999	pink	gneissic	-9999	phaneritic fine (0.5-1mm)	No notes captured.	minor lithology	mafic rocks	amphibolite	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Mafic enclaves? Is the mafic component here the same as mafic banding in 2057?	FOL - Foliation	237	90	Foliation weak	LS fabric; more lineation and less foliation seen.	FT - Fault Brittle	53	86	-9999	Faults trending 053/86, plunging 12 -> 21, latest fault movement?	-9999	-9999	-9999	-9999	-9999	LL-23-2058-1	whole-rock lithogeochemistry	Orthogneiss.	LL-23-2058-2	whole-rock lithogeochemistry	Amphibolite mafic enclave.	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2059	01-07-2023 10:41:26.474	59.752968	-111.100026	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Orthogneiss (white weathering) potential paleosome reflects dominant lithology with interlayered foliated granite. Mafic xenoliths of potential gabbro present within orthogneiss. Xenoliths have biotite/hornblende envelope about 1cm wide, interior is coarse-grained amphibolite with supracrustal appearance (i.e. gritty, sedimentary/volcanic xenoliths?).	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	buff grey	gneissic	migmatitic	phaneritic fine (0.5-1mm)	Multiple phases of granite with respect to grain size; pervasive folding of all three units.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	AXF - Axial fold plane	245	74	-9999	General hinge line 74 towards 245.	-9999	-9999	-9999	-9999	-9999	FOL - Foliation	260	63	-9999	-9999	LL-23-2059-1	whole-rock lithogeochemistry	Granite leucosome of the main lithology (orthogneiss).	LL-23-2059-2	whole-rock lithogeochemistry	Mafic xenolith.	LL-23-2059-3	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2060	01-07-2023 11:47:35.792	59.754218	-111.095856	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Rusty gossan at shoreline of probable sedimentary origin.  Abundant isoclinal S folds throughout outcrop; rusty zones parallel to folds. Granite is folded with orthogneiss or could be nosing it’s way into fold hinges.	main lithology	gneiss	orthogneiss	biotite	-9999	hornblende	-9999	alkali-feldspar	-9999	buff grey	-9999	migmatitic	-9999	Sharp contacts with granite components; lithologies at not as mixed here. Mafic component has greenish tint. Pyritic sheen. Quartz and potential cordierite. Highly strained (mylonitic).	minor lithology	granitoid	granite	-9999	-9999	-9999	-9999	-9999	-9999	pink	-9999	-9999	-9999	Sills and layers of granite within orthogneiss.	AXF - Axial fold plane	52	84	-9999	Trend 048, plunging 71 (plunging 71 towards 48). Third fold 60 -> 065, axial plane 245/70.	FOL - Foliation	235	70	-9999	-9999	AXF - Axial fold plane	236	70	-9999	Fold 2: 76 -> 055.	LL-23-2060-1	whole-rock lithogeochemistry; oriented thin section	Oriented sulphide bearing mafic component of orthogneiss, or is this paragneiss?	LL-23-2060-2	whole-rock lithogeochemistry	White weathering orthogneiss.	LL-23-2060-3	whole-rock lithogeochemistry	Pink weathered granite, massive to weakly foliated.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2061	02-07-2023 10:30:40.342	59.795015	-111.039876	Internal GPS	Nicholas Montenegro	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Orthogneiss, 3 components. White weathering with biotite rich laminate best expressing the structural style, inter layered with alkali feldspar granite and biotite rich(?) or amphibolite layers/enclaves. Sample LL-23-2061-3 reflects mafic component. Leucosomal quartz and feldspar veins.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	FOL1 - Foliation gen1	193	90	Foliation strong	Mylonitic.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2061-1	whole-rock lithogeochemistry	White weathering,  biotite laminae component of orthogneiss.	LL-23-2061-2	whole-rock lithogeochemistry	Pink weathering, alkali feldspar granite component.	LL-23-2061-3	whole-rock lithogeochemistry	Amphibolite enclave.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2062	02-07-2023 11:10:11.544	59.790719	-111.047313	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alkali feldspar granite and small chunks of main white weathering orthogneiss component in LL-23-2062-1.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	dominated by pink weathering  	-9999	-9999	-9999	Mafic enclaves present (both rounded and strung out along foliation). Seeing 10cm wide layers of white pseudotachyllite? Appears late and is infilling fractures oriented 130/90. Foliation only apparent in some areas, where more of the original orthogneiss component exists and displays biotite laminae/enclaves. Low cps, background of 200.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2062-1	whole-rock lithogeochemistry	Orthogneiss, large chunk is of the alkali feldspar granite component. Small fragments of primary gneissic, white weathering component.	LL-23-2062-2	whole-rock lithogeochemistry	White weathered component running along fractures in orthogneiss pseudotachylite.	LL-23-2062-3	whole-rock lithogeochemistry	Mafic enclave component. Extremely hematized.	-9999	-9999	-9999	Alberta Geological Survey
LL-23-2063	02-07-2023 12:43:43.227	59.783613	-111.060119	Internal GPS	Courtney Reimert	Nicholas Montenegro	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	main lithology	gneiss	orthogneiss	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	No notes captured.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	LL-23-2063-1	whole-rock lithogeochemistry	Orthogneiss.	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
