Sample_ID	Samp_type	UWI_label	Well_name	Lat_NAD83	Long_NAD83	KB_el_m28	Depth_m	Domain	Gen_lith	Lithology	Textures	Descrip	Qz_pct	Pl_pct	Afs_pct	Opx_pct	Cpx_pct	Amp_pct	Bt_pct	Grt_pct	Ms_pct	Chl_pct	Ep_pct	Sil_pct	Crd_pct	And_pct	Cal_pct	Opq_pct	Zrn_pct	Mnz_pct	Ap_pct	Aln_pct	Ttn_pct	Publisher
24BA001	drillcore	100/10-10-075-08W6/00	SPOKE RESOURCES VALHALLA 10-10-75-8	55.486167	-119.146145	828.8	3519.52	Ksituan	granitoid	granite	Intensely altered, medium-grained, equigranular, phaneritic	Intensely altered, sericitized granite. Some feldspar crystals are completely replaced with fine-grained sericite preserving their relict shape. Opaque minerals are often intergrown with long, acicular to locally radial mica. Long, tabular to wedge-shaped zircon. Thin, 0.1-0.2 mm wide, sericite-filled fractures.	32	5	23	-9999	-9999	-9999	-9999	-9999	19	5	-9999	-9999	-9999	-9999	-9999	15	1	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA002	drillcore	100/10-10-075-08W6/00	SPOKE RESOURCES VALHALLA 10-10-75-8	55.486167	-119.146145	828.8	3526.10	Ksituan	granitoid	biotite-amphibole granite	Moderately sericite altered, medium-grained, equigranular, phaneritic	Moderately sericitized granite. Moderately sericitized, subhedral plagioclase and weakly sericitized, subhedral alkali feldspar with anhedral quartz. Sericite alteration is often concentrated at the core of the grains and extends outwards to the grain edges. Abundant titanite often concentrated along the rims of opaque minerals. Clusters of apatite often hosted within hornblende and biotite. 	15	23	28	-9999	-9999	15	7	-9999	5	-9999	-9999	-9999	-9999	-9999	-9999	3	tr	tr	1	tr	3	Alberta Geological Survey
24BA003	drillcore	100/15-34-043-10W4/00	PCP KILLAM 15-34-43-10	52.755110	-111.365940	672.5	2147.73	Loverna	metavolcanic	basaltic andesite	Foliated, poikilitic, very fine grained, equigranular, aphanitic	Foliated, very fine grained basaltic andesite. Subhedral amphibole set in a finer-grained matrix of anhedral plagioclase and lesser quartz. Occasional larger (up to 1 mm) plagioclase contains inclusions of biotite (poikilitic). Weak calcite alteration replaces individual grains and forms discontinuous veinlets.	10	52	-9999	-9999	-9999	35	tr	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	3	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA004	drillcore	100/01-31-013-20W4/00	SLE ET AL ROBIN 1-31-13-20	50.123498	-112.715436	895.9	2556.30	Medicine Hat	granitoid	amphibole-biotite tonalite	Medium-grained, inequigranular, phaneritic, granophyric	Medium-grained amphibole-biotite tonalite. Anhedral, plagioclase and quartz form the bulk of the rock with average crystal sizes between 1-3 mm. Occasional granophyric intergrowth texture. Anhedral plagioclase and biotite often form clusters with zircon and apatite. Rare, intensely altered allanite.	42	36	-9999	-9999	-9999	8	10	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	tr	tr	-9999	Alberta Geological Survey
24BA005	drillcore	100/16-19-116-04W6/00	OVV ZAMA 16-19-116-4	59.094800	-118.658007	380.4	1727.20	Hottah	dioritoid	biotite quartz diorite	Medium-grained, equigranular, phaneritic	Medium-grained biotite quartz diorite. Plagioclase crystals contain occasional patches of sericite alteration in their cores. Embayed epidote with ragged margins replacing plagioclase.	11	48	-9999	-9999	-9999	4	28	-9999	4	-9999	5	-9999	-9999	-9999	-9999	-9999	tr	-9999	tr	-9999	tr	Alberta Geological Survey
24BA006	drillcore	100/15-23-079-16W5/00	Baytex Energy Ltd.	55.866200	-116.384522	680.9	2039.45	Buffalo High	granitoid	biotite alkali feldspar granite	Medium-grained, porphyritic, inequigranular, phaneritic, granophyric	Medium-grained, biotite alkali feldspar granite. Tabular, subhedral alkali feldspar phenocrysts (up to 10 mm long) with perthitic texture are set in a 0.5-2 mm matrix of mainly quartz, plagioclase, and biotite. Feldspars are weakly altered to fine-grained sericite, while plagioclase is altered to epidote with ragged margins.	20	6	60	-9999	-9999	-9999	10	-9999	1	-9999	1	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA007	drillcore	103/03-04-057-20W4/00	SCL REDWATER 3-4-57-20	53.893186	-112.915159	613.2	2115.40	Rimbey	granitoid	granodiorite	Coarse-grained, porphyritic, inequigranular, antiperthite	Coarse-grained, inequigranular granodiorite. Anhedral, strained, plagioclase crystals form the bulk of the sample, are generally 6 to 8 mm long, and contain antiperthite. Anhedral alkali feldspar and quartz crystals are smaller (0.5 to 2 mm). Biotite commonly forms clusters (individual crystals up to 3 mm long) and is altered to chlorite and opaque minerals, with ragged edges. 	24	58	8	-9999	-9999	-9999	4	-9999	2	4	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA008	drillcore	103/03-04-057-20W4/00	SCL REDWATER 3-4-57-20	53.893186	-112.915159	613.2	2117.00	Rimbey	granitoid	granodiorite	Fine-grained, equigranular, antiperthite	Fine-grained, equigranular granodiorite. Primarily composed of 0.5-2 mm plagioclase and quartz with lesser alkali feldspar. Tabular biotite is altered to chlorite with ragged edges. Chlorite also partially replaces 0.5 mm garnet along fractures and margins. A thin (~200 m) veinlet with a calcite core and sericite-chlorite rims transects the section.	46	28	8	-9999	-9999	-9999	3	4	2	4	-9999	-9999	-9999	-9999	1	4	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA009	drillcore	100/01-19-083-09W5/00	AEL WAINOCO UTIKUMA 1-19-83-9	56.205133	-115.403385	682.8	1753.10	Buffalo Utikuma	granitoid	biotite granodiorite	Moderately altered, coarse-grained, porphyritic, inequigranular	Coarse-grained, plagioclase-phyric, biotite granodiorite. Tabular plagioclase crystals (0.2-10 mm) are altered to blebby brown biotite and alkali feldspar, producing ragged margins. Quartz and alkali feldspar are comparatively less altered. Very fine grained sericite fills fractures and locally replaces plagioclase.	30	13	20	-9999	-9999	-9999	35	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA010	drillcore	100/01-19-083-09W5/00	AEL WAINOCO UTIKUMA 1-19-83-9	56.205133	-115.403385	682.8	1755.10	Buffalo Utikuma	granitoid	biotite granodiorite	Coarse-grained, porphyritic, inequigranular	Coarse-grained, plagioclase-phyric, biotite granodiorite. Tabular plagioclase phenocrysts (up to 10 mm long) are set in a finer-grained matrix of mainly plagioclase and quartz (0.5-1 mm). Biotite forms a wispy, interstitial texture that wraps around plagioclase phenocrysts.	30	45	5	-9999	-9999	-9999	20	-9999	tr	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA011	drillcore	100/10-13-060-04W4/00	TEXEX ET AL CHAR LAKE 10-13-60-4	54.189649	-110.463783	601.4	1435.70	Loverna	granitoid	biotite tonalite	Medium-grained, inequigranular	Medium-grained biotite tonalite. Mainly composed of anhedral quartz (0.5-4 mm) and plagioclase (1-3 mm) with rare anhedral alkali feldspar crystals. Clusters of biotite with lesser, very fine grained muscovite.	40	40	3	-9999	-9999	-9999	15	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA012	drillcore	100/04-14-076-22W5/00	NRL77 GVILLEE 4-14-76-22	55.579719	-117.307638	556.0	2453.26	Buffalo Arch	granitoid	granite	Altered, sericitization, chloritization, fine-grained, equigranular	Sericite-chlorite altered, fine-grained granite. Composed of 0.2-0.5 mm, anhedral quartz and alkali feldspar with lesser 0.2-0.5 mm, anhedral plagioclase. Feldspars are sericitized, often with more intense alteration in crystal cores. Platy, anhedral chlorite is often associated with equant opaque minerals.	37	15	33	-9999	-9999	-9999	-9999	-9999	3	4	-9999	-9999	-9999	-9999	-9999	8	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA013	drillcore	100/09-10-088-03W5/00	MURPHY TOTAL PEERLESS LAKE 9-10-88-3	56.620251	-114.379484	740.0	1461.55	Buffalo Utikuma	metasedimentary	quartzite	Medium-grained, equigranular, granoblastic	Medium-grained quartzite. Quartz is anhedral, 1-4 mm in width displaying granoblastic texture. Rare, platy muscovite and biotite. 	99	-9999	-9999	-9999	-9999	-9999	tr	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA014	drillcore	100/11-29-088-23W5/00	OAK ET AL LONESTAR 11-29-88-23	56.663878	-117.635349	636.9	1974.55	Buffalo High	granitoid	granite	Altered, veined, fine-grained, inequigranular	Moderately altered, veined, fine-grained, inequigranular granite. Host rock composed of anhedral, 0.2-0.5 mm quartz, alkali feldspar, and plagioclase. Opaque minerals occur as equant, subhedral, 0.5 mm crystals, as well as pervasive, dendritic stringers defining foliation. Anhedral chlorite with ragged margins is common with occasional overprinting patches up to 4 mm in size. Several generations of quartz veining including: 1) Early, thin (roughly 0.5 mm) quartz veins. 2) Wider (roughly 8 mm), discontinuous, opaque mineral-biotite-quartz veins, and 3) late, 4 mm wide, anastomosing quartz veins.	30	15	16	-9999	-9999	-9999	5	-9999	-9999	16	-9999	-9999	-9999	-9999	-9999	18	-9999	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA015	drillcore	100/11-29-088-23W5/00	OAK ET AL LONESTAR 11-29-88-23	56.663878	-117.635349	636.9	1974.85	Buffalo High	granitoid	granite	Altered, veined, sericitized, fine-grained, inequigranular	Moderately altered, inequigranular, fine-grained granite with quartz veining. Very fine grained matrix is composed of anhedral alkali feldspar, quartz, and plagioclase (50-100 m). Alkali feldspar phenocrysts (up to 8 mm) contain healed fractures. Very fine grained sericite replaces feldspar and overprints fine-grained matrix of the host rock. Disseminated, anhedral chlorite with ragged margins. Occasional, discontinuous quartz veins up to 1 mm wide.	25	20	30	-9999	-9999	-9999	-9999	-9999	17	5	-9999	-9999	-9999	-9999	-9999	3	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA016	drillcore	1AA/06-08-066-02W4/00	ESSO MEDLEY OV 6-8-66-2	54.695154	-110.272779	613.8	1215.83	Loverna	granitoid	alkali feldspar granite	Altered, fine-grained, inequigranular	Fine-grained, inequigranular alkali feldspar granite with a bimodal grain size distribution. Anhedral quartz (0.5-2 mm) set in matrix of anhedral alkali feldspar (0.2-0.5 mm). Platy, 0.5 mm long, anhedral biotite and muscovite. Abundant, anhedral calcite with ragged edges replacing primary minerals and filling interstitial spaces. Very fine grained, dendritic to equant opaque minerals.	38	-9999	45	-9999	-9999	-9999	5	-9999	3	-9999	-9999	-9999	-9999	-9999	8	1	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA017	drillcore	103/07-11-059-20W4/00	SCL RADWAY 7-11-59-20	54.085174	-112.886521	641.4	2062.38	Rimbey	gneiss	biotite-hornblende gneiss	Saussuritization, banded, foliated, fine-grained, inequigranular	Banded (0.5-1 cm), fine-grained biotite-hornblende gneiss. Leucosomes comprise anhedral plagioclase (0.5-1 mm), quartz (0.3-3 mm), and alkali feldspar (0.5 mm). Melanosomes comprise anhedral to subhedral, tabular hornblende and platy biotite, both up to 2 mm long. Minor alteration of feldspar to epidote and sericite.	23	35	10	-9999	-9999	17	11	-9999	2	tr	2	-9999	-9999	-9999	-9999	-9999	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA018	drillcore	103/07-11-059-20W4/00	SCL RADWAY 7-11-59-20	54.085174	-112.886521	641.4	2063.13	Rimbey	gneiss	biotite gneiss	Saussuritization, banded, foliated, medium-grained, inequigranular	Banded, foliated, medium-grained biotite gneiss. Leucosomes are approximately 1 cm wide, while melanosomes are much thinner. Leucosomes comprise of anhedral quartz (0.2-4 mm), plagioclase (0.5-3 mm), and alkali feldspar (0.5-1 mm). Melanosomes comprise subhedral, platy biotite up to 3 mm long. Weak alteration of feldspar and biotite to epidote with ragged margins. Biotite is locally altered to chlorite.	35	25	23	-9999	-9999	-9999	15	-9999	-9999	tr	2	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA019	drillcore	1AA/12-10-098-03W4/00	SILVERBIRCH AUDET 12-10-98-3	57.491093	-110.407260	485.0	202.12	Rae	granitoid	biotite alkali feldspar granite	Medium-grained, inequigranular, porphyritic, granophyric	Porphyritic, medium-grained biotite alkali feldspar granite. Phenocrysts comprise anhedral quartz (up to 4 mm) and subhedral alkali feldspar (up to 6 mm). Finer grained matrix comprises alkali feldspar and quartz (50-400 m) with minor plagioclase. Biotite occurs in patches of platy grains up to 0.5 mm long. Feldspar is locally altered to sericite, which forms bands within feldspar grains.	38	3	48	-9999	-9999	-9999	7	-9999	3	-9999	-9999	-9999	-9999	-9999	-9999	1	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA020	drillcore	100/07-05-085-11W4/00	SUNCOR ET AL HANGSTN 7-5-85-11	56.338844	-111.703607	541.8	842.45	Taltson Charles Lake - Athabasca	granitoid	garnet-biotite granodiorite	Medium-grained, inequigranular, porphyritic, granophyric	Medium-grained, inequigranular garnet-biotite granodiorite. Comprised of anhedral plagioclase, quartz, and minor alkali feldspar. Biotite as disseminated clusters and fracture-fill. Phenocrysts of equant, subhedral, fractured garnets up to 6 mm wide. One discontinuous quartz-muscovite vein (0.5 mm wide), with local zoning.	25	38	5	-9999	-9999	-9999	15	13	2	-9999	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA021	drillcore	100/02-31-093-02W5/00	GULF SENEX 2-31-93-2	57.106945	-114.304935	657.6	1348.90	Buffalo Utikuma	gabbroid	gabbro	Fine-grained, equigranular	Fine-grained, equigranular gabbro. Comprises anhedral plagioclase (0.3-0.6 mm), subhedral orthopyroxene (0.5-1 mm), and subhedral clinopyroxene (0.5-1 mm). Orthopyroxene is altered to chlorite and opaque minerals along fractures and cleavage planes. Lesser anhedral amphiboles (up to 1 mm long) and equant to interstitial opaque minerals (0.5-1 mm). 	-9999	40	-9999	18	20	7	-9999	-9999	-9999	1	-9999	-9999	-9999	-9999	-9999	14	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA022	drillcore	100/02-31-093-02W5/00	GULF SENEX 2-31-93-2	57.106945	-114.304935	657.6	1352.90	Buffalo Utikuma	charnockitoid	biotite jotunite	Medium- to coarse-grained, inequigranular, phaneritic	Medium- to coarse-grained, inequigranular biotite jotunite. Comprises anhedral plagioclase (1-5 mm) with lesser, anhedral alkali feldspar (1-5 mm) and subhedral orthopyroxene (0.5-1 mm). Orthopyroxene is spatially associated with clusters of anhedral biotite (up to 1 mm long) and very fine grained opaque minerals. Orthopyroxene alters to chlorite along fractures and cleavage planes.	-9999	62	14	13	-9999	-9999	7	-9999	2	2	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA023	drillcore	100/02-31-093-02W5/00	GULF SENEX 2-31-93-2	57.106945	-114.304935	657.6	1359.90	Buffalo Utikuma	charnockitoid	biotite jotunite	Coarse-grained, inequigranular, phaneritic	Coarse-grained, inequigranular biotite jotunite. Comprises anhedral plagioclase (0.5-10 mm) with lesser anhedral alkali feldspar (0.5-4 mm), subhedral, equant orthopyroxene (0.5-3 mm), and anhedral quartz (0.5-1 mm). Plagioclase is locally altered to sericite, which forms bands within feldspar grains. Orthopyroxene is partially to completely altered to biotite, chlorite, and opaque minerals. 	4	64	13	10	-9999	-9999	5	-9999	1	3	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA024	drillcore	100/09-22-082-12W4/00	CLL DIVIDE 9-22-82-12	56.125171	-111.780986	765.2	1106.18	Taltson South	granitoid	biotite granite	Medium-grained, inequigranular, phaneritic, porphyritic, granophyric	Medium-grained, porphyritic biotite granite with bimodal grain size distribution. Phenocrysts (1-5 mm) comprise quartz, alkali feldspar, and minor plagioclase set in matrix of quartz, plagioclase, and lesser alkali feldspar. Biotite occurs as clusters of fine-grained, platy crystals.	45	21	29	-9999	-9999	-9999	5	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA025	drillcore	100/09-22-082-12W4/00	CLL DIVIDE 9-22-82-12	56.125171	-111.780986	765.2	1111.00	Taltson South	granitoid	biotite granodiorite	Medium-grained, inequigranular, phaneritic, porphyritic, granophyric, foliated	Medium-grained, porphyritic biotite granodiorite. Phenocrysts (1-5 mm) of quartz, plagioclase, and lesser alkali feldspar are set in a fine-grained (0.2 mm) matrix of quartz, plagioclase, and alkali feldspar. Biotite forms fine-grained bands and clusters that locally define interstitial fabric around larger phenocrysts. Biotite is altered to chlorite and calcite, forming anhedral patches with ragged margins that are spatially associated with opaque minerals. 	30	30	10	-9999	-9999	-9999	22	-9999	-9999	5	-9999	-9999	-9999	-9999	2	1	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA026	drillcore	100/13-11-116-08W6/00	IMPERIAL AMBER 13-11-116-8	59.065202	-119.248878	408.1	1846.80	Hottah	metavolcanic	intermediate metavolcanic rock	Banded, very fine grained, inequigranular, aphanitic, poikilitic	Banded, very fine grained to aphanitic intermediate metavolcanic rock. Comprises anhedral plagioclase (0.2-2 mm) with lesser quartz and tabular to acicular amphibole (50-200 m). Plagioclase often encloses multiple amphibole crystals, forming a poikilitic texture. Disseminated anhedral chlorite with ragged margins and minor amounts of opaque minerals and epidote. Occasional <1 mm to 5 mm quartz veinlets.	15	35	-9999	-9999	-9999	35	-9999	-9999	-9999	10	3	-9999	-9999	-9999	-9999	2	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA027	drillcore	100/13-20-085-02W5/00	SHELL TROUT 13-20-85-2	56.388713	-114.287609	698.7	1620.40	Buffalo Utikuma	gneiss	biotite gneiss	Foliated, banded, medium-grained, inequigranular, phaneritic, granophyric	Heavily altered, medium-grained, inequigranular biotite gneiss. Leucosomes composed of anhedral quartz, plagioclase, and alkali feldspar (0.05-5 mm). Melanosomes composed of anhedral to subhedral biotite (up to 1 mm long). Feldspars partially or completely altered to sericite. Biotite alteration spatially associated with opaque minerals and minor chlorite. Thin, sub-millimetre quartz veinlets spatially associated with alteration.	27	21	14	-9999	-9999	-9999	18	-9999	10	3	-9999	-9999	-9999	-9999	tr	7	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA028	drillcore	100/12-23-092-16W5/00	IOE JACKPINE 12-23-92-16	56.998843	-116.465384	710.8	1789.40	Buffalo High	gneiss	biotite-orthopyroxene-alkali feldspar gneiss	Banded, fine- to medium-grained, inequigranular, phaneritic, granophyric	Fine- to medium-grained, inequigranular biotite-orthopyroxene-alkali feldspar gneiss. Primarily composed anhedral alkali feldspar (0.3-2 mm) with minor quartz. Clusters of biotite altered to chlorite, subhedral orthopyroxene, and equant opaque minerals form an interstitial fabric around larger alkali feldspar crystals.	3	-9999	52	17	-9999	-9999	7	-9999	-9999	7	-9999	-9999	-9999	-9999	-9999	13	-9999	-9999	1	-9999	-9999	Alberta Geological Survey
24BA029	drillcore	100/12-23-092-16W5/00	IOE JACKPINE 12-23-92-16	56.998843	-116.465384	710.8	1793.06	Buffalo High	gneiss	biotite gneiss	Foliated, banded, medium-grained, inequigranular, phaneritic, granophyric	Weakly to moderately altered, medium-grained biotite gneiss. Primarily composed of anhedral quartz, alkali feldspar, and plagioclase. Alkali feldspar and plagioclase occur in separate bands. Feldspars altered to sericite. Minor subhedral biotite (up to 1 mm long) occurs as aggregates and commonly partially to completely altered to chlorite. 	44	14	29	-9999	-9999	-9999	2	-9999	8	1	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA030	drillcore	102/10-08-099-13W5/00	HONOLULU MOBIL BUFFALO A10-8-99-13	57.578817	-116.091571	687.6	1716.00	Buffalo High	gneiss	hornblende-biotite gneiss	Medium-grained, equigranular, phaneritic	Medium-grained hornblende-biotite gneiss. Leucosomes composed primarily of plagioclase and quartz with minor alkali feldspar. Melanosomes composed of biotite and hornblende (up to 2 mm long). Weak alteration to chlorite. Disseminated, equant to interstitial opaque minerals.	25	44	3	-9999	-9999	10	13	-9999	-9999	1	-9999	-9999	-9999	-9999	-9999	3	tr	-9999	1	-9999	-9999	Alberta Geological Survey
24BA031	drillcore	100/13-09-086-21W4/00	TRITON ET AL BUFFALO 13-9-86-21	56.446358	-113.265010	578.2	1206.65	Taltson Slave - Birch	gneiss	garnet-biotite-andalusite gneiss	Banded, intensely altered, fine- to medium-grained, inequigranular, phaneritic	Intensely altered, weakly banded, fine- to medium-grained garnet-biotite-andalusite gneiss. Anhedral alkali feldspar and quartz (0.1-4 mm). Platy biotite (up to 0.5 mm long) and subhedral garnet (up to 4 mm) with fractured crystals. Equant, subhedral andalusite (0.5 mm) with partial alteration to sericite and locally included by opaque minerals. Sericite completely replaces unidentified relict crystals (up to 4 mm).	36	-9999	25	-9999	-9999	-9999	8	6	10	-9999	-9999	-9999	-9999	12	-9999	3	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA032	drillcore	100/06-33-099-07W5/02	CALSTAN SENEX CREEK 6-33-99-7	57.633907	-115.085558	407.5	1222.10	Buffalo Utikuma	gneiss	biotite gneiss	Moderately altered, banded, medium-grained, inequigranular, phaneritic	Moderately altered, medium-grained biotite gneiss. Leucosomes composed of anhedral quartz, alkali feldspar, and plagioclase (0.2-8 mm). Melanosomes composed of disseminated biotite that is partially altered to chlorite with ragged margins. Plagioclase is commonly completely altered to very fine grained sericite.	27	10	35	-9999	-9999	-9999	3	-9999	18	7	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA033	drillcore	100/10-06-091-01W5/00	IOE LIEGE RIVER 10-6-91-1	56.866403	-114.146678	592.2	1309.45	Buffalo Utikuma	granitoid	biotite alkali feldspar granite	Moderately altered, fine- to medium-grained, inequigranular, phaneritic	Moderately altered, fine- to medium-grained biotite alkali feldspar granite. Bimodal grain size distribution of quartz and alkali feldspar consisting of a anhedral to subhedral crystals (up to 4 mm) set in a fine-grained (0.1-0.3 mm) matrix. Occasional, subhedral garnets (up to 2 mm) with commonly fractured crystals. Alkali feldspar is partially altered to very fine grained sericite. Biotite completely altered to chlorite. Chlorite and biotite form very thin veinlets (<0.5 mm wide).	45	-9999	27	-9999	-9999	-9999	8	3	3	8	-9999	-9999	-9999	-9999	-9999	5	1	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA034	drillcore	100/10-18-081-06W5/00	ATLANTIC MUSKWA 10-18-81-6	56.023533	-114.923850	652.9	1762.51	Buffalo Utikuma	gneiss	biotite gneiss	Banded, foliated, moderately altered, fine-grained, inequigranular, phaneritic	Banded (~1 cm wide), moderately altered, fine-grained biotite gneiss. Leucosomes composed of anhedral to subhedral quartz, plagioclase, and lesser alkali feldspar (0.1-4 mm). Melanosomes composed primarily of platy biotite that is partially to completely altered to chlorite. Feldspars are partially altered by sericite. Occasional, thin (<1 mm) quartz veinlets.	25	36	15	-9999	-9999	-9999	12	-9999	7	5	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA035	drillcore	100/10-23-086-09W6/00	SHELL WORSLEY 10-23-86-9	56.474068	-119.301739	637.6	2289.43	Ksituan	gneiss	biotite gneiss	Banded, foliated, moderately altered, porphyritic, fine-grained, inequigranular	Moderately altered, fine-grained, porphyritic biotite gneiss. Clusters of quartz, alkali feldspar, and plagioclase phenocrysts set in a microcrystalline matrix of quartz, alkali feldspar, plagioclase. Phenocrysts partially altered to calcite and sericite. Weak, disseminated alteration of matrix to chlorite, muscovite, and calcite. Occasional euhedral, equant opaque minerals.	34	14	24	-9999	-9999	-9999	3	-9999	5	9	-9999	-9999	-9999	-9999	10	1	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA036	drillcore	100/14-36-080-10W5/00	AMOCO A-6 UTIKUMA 14-36-80-10	55.983146	-115.426938	656.2	1691.48	Buffalo Utikuma	gneiss	biotite gneiss	Banded, foliated, moderately altered, fine-grained, inequigranular, phaneritic	Moderately altered, thinly banded (0.2-0.5 cm), fine-grained biotite gneiss. Leucosomes composed of anhedral quartz, alkali feldspar, and plagioclase (0.5-2 mm). Feldspars partially to completely altered to sericite. Biotite altered to chlorite. Calcite completely replacing some grains. Thin (<1 mm), chaotic calcite veinlets. Opaque minerals as equant crystals and infill thin (<1 mm), chaotic, anastomosing veinlets.	25	30	20	-9999	-9999	-9999	5	-9999	10	3	-9999	-9999	-9999	-9999	4	3	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA037	drillcore	100/02-02-080-06W5/00	TEXCAN ET AL MCCONACHIE 2-2-80-6	55.899607	-114.819426	642.8	1762.64	Buffalo Utikuma	gneiss	biotite-hornblende gneiss	Banded, foliated, weakly altered, fine-grained, inequigranular, phaneritic	Weakly altered, well banded (0.5-1 cm), fine-grained biotite-hornblende gneiss. Leucosomes composed of plagioclase and quartz with minor alkali feldspar (0.2-4 mm). Melanosomes composed of hornblende (0.5-2 mm long) and platy, subhedral biotite (up to 1 mm long). Hornblende partially to completely altered to calcite. Occasional patches and veinlets of chlorite along with disseminated, anhedral opaque minerals.	21	40	3	-9999	-9999	15	10	-9999	2	2	-9999	-9999	-9999	-9999	4	3	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA038	drillcore	100/02-02-080-06W5/00	TEXCAN ET AL MCCONACHIE 2-2-80-6	55.899607	-114.819426	642.8	1763.34	Buffalo Utikuma	granitoid	granite	Foliated, fine- to medium-grained, equigranular, phaneritic	Foliated, fine- to medium-grained granite. Composed of anhedral quartz and alkali feldspar (0.5-4 mm) with lesser plagioclase. Feldspars weakly altered to sericite. Minor patchy chlorite and biotite alteration along with thin (<1 mm), discontinuous veinlets.	35	10	52	-9999	-9999	-9999	tr	-9999	2	1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA039	drillcore	100/02-02-080-06W5/00	TEXCAN ET AL MCCONACHIE 2-2-80-6	55.899607	-114.819426	642.8	1765.59	Buffalo Utikuma	gneiss	biotite-hornblende gneiss	Banded, foliated, weakly altered, fine- to medium-grained, inequigranular, phaneritic, granophyric	Weakly altered, discontinuously banded (0.5-1 cm), fine- to medium-grained biotite-hornblende gneiss. Leucosomes composed of anhedral quartz and plagioclase (0.25-4 mm). Melanosomes composed of tabular hornblende and platy biotite. Feldspars are weakly altered to very fine grained sericite. Amphiboles partially altered to calcite, chlorite, and trace epidote.	24	37	-9999	-9999	-9999	18	12	-9999	2	1	tr	-9999	-9999	-9999	4	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA040	drillcore	100/08-09-079-11W5/00	SUMMERLAND GIFT 8-9-79-11	55.829599	-115.645278	698.7	1886.45	Buffalo Utikuma	dioritoid	quartz monzodiorite	Weakly altered, fine-grained, equigranular, phaneritic	Weakly altered, fine-grained quartz monzodiorite. Primarily composed of anhedral plagioclase and alkali feldspar (0.5-1 mm) with minor quartz. Feldspar partially to completely altered to very fine grained sericite. Opaque minerals rim the margins of altered feldspar crystals. Disseminated anhedral chlorite with ragged margins. Thin (<1 mm) calcite veinlets.	5	57	20	-9999	-9999	-9999	-9999	-9999	10	5	-9999	-9999	-9999	-9999	1	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA041	drillcore	100/08-09-079-11W5/00	SUMMERLAND GIFT 8-9-79-11	55.829599	-115.645278	698.7	1892.40	Buffalo Utikuma	gneiss	epidote-chlorite-bearing gneiss	Foliated, weakly altered, fine-grained, equigranular, phaneritic	Weakly altered, fine-grained epidote-chlorite-bearing gneiss. Composed of anhedral quartz and alkali feldspar (0.05-2 mm). Clusters of anhedral chlorite and epidote with ragged margins along with lesser, disseminated opaque minerals.	65	-9999	15	-9999	-9999	-9999	-9999	-9999	-9999	8	8	-9999	-9999	-9999	-9999	4	tr	tr	tr	-9999	-9999	Alberta Geological Survey
24BA042	drillcore	100/13-20-075-02W6/00	CHEVRON SMOKEY R 13-20-75-2	55.517703	-118.281525	645.3	2929.30	Ksituan	gneiss	hornblende gneiss	Foliated, weakly altered, fine-grained, equigranular, phaneritic	Weakly altered, banded (5-10 mm), fine-grained hornblende gneiss. Leucosomes composed of anhedral to subhedral alkali feldspar (0.2-4 mm) with lesser anhedral quartz and plagioclase (0.1-1 mm). Melanosomes dominantly composed of subhedral, tabular hornblende (up to 2 mm long), weakly altered to chlorite and calcite. Anhedral opaque minerals (up to 2 mm) commonly associated with titanite.	15	15	35	-9999	-9999	28	1	-9999	-9999	1	-9999	-9999	-9999	-9999	tr	4	tr	-9999	tr	-9999	1	Alberta Geological Survey
24BA043	drillcore	102/01-14-059-10W4/00	CNRL 102 CACHE 1-14-59-10	54.096746	-111.379149	651.1	1709.89	Loverna	granitoid	garnet-hornblende-muscovite-biotite granite	Medium-grained, inequigranular, porphyritic, phaneritic	Medium-grained garnet-hornblende-muscovite-biotite granite. Occasional, euhedral alkali feldspar phenocrysts (1 cm long) set in a medium-grained matrix composed primarily of anhedral to subhedral alkali feldspar, plagioclase, and quartz. Biotite and muscovite as platy aggregates (up to 1 mm long). Rare, equant garnet (up to 2 mm) and rare tabular hornblende. 	27	20	38	-9999	-9999	1	10	1	3	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA044	drillcore	102/01-14-059-10W4/00	CNRL 102 CACHE 1-14-59-10	54.096746	-111.379149	651.1	1718.65	Loverna	granitoid	muscovite-biotite granite	Medium-grained, inequigranular, phaneritic, granophyric.	Medium-grained muscovite-biotite granite. Primarily composed of anhedral to subhedral alkali feldspar (up to 10 mm long), quartz (1-4 mm), and plagioclase (1-4 mm). Minor platy biotite (up to 1.5 mm long) and muscovite (up to 4 mm long). 	28	20	40	-9999	-9999	-9999	8	-9999	4	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	tr	-9999	-9999	Alberta Geological Survey
24BA045	drillcore	100/07-18-083-14W5/00	HUSKY ET AL SEAL 7-18-83-14	56.195193	-116.196966	709.5	1790.29	Buffalo High	granitoid	biotite granite	Medium- to coarse-grained, inequigranular, phaneritic, granophyric	Medium- to coarse-grained biotite granite. Primarily composed of anhedral to subhedral alkali feldspar, quartz, and plagioclase (0.2-10 mm). Feldspars weakly to moderately altered to sericite. Platy, subhedral biotite (up to 0.5 mm long) partially altered to chlorite exhibiting ragged margins.	25	20	38	-9999	-9999	-9999	10	-9999	5	2	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA046	drillcore	100/10-10-066-06W4/00	BP LEMING 10-10-66-6	54.699699	-110.820299	632.6	1352.56	Loverna	metasedimentary	garnet-sillimanite-cordierite-biotite schist	Foliated, fine-grained, inequigranular, phaneritic, porphyroblastic	Foliated, fine-grained garnet-sillimanite-cordierite-biotite schist. Composed primarily of abundant, platy biotite (up to 1 mm long), anhedral quartz (0.2-1 mm), and anhedral plagioclase (0.2-1 mm). Biotite spatially associated with mats of very fine grained acicular sillimanite. Garnet occurs as euhedral, equant porphyroblasts (up to 3 mm) that exhibit augen-like texture. Cordierite occurs as porphyroblasts (up to 5 mm) that are partially altered to pinite and contain inclusions of biotite, sillimanite, and quartz (poikilitic texture). Occasional subhedral, equant to tabular opaque minerals spatially association with biotite.	26	12	-9999	-9999	-9999	-9999	28	7	-9999	-9999	-9999	12	12	-9999	-9999	3	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA047	drillcore	100/10-10-066-06W4/00	BP LEMING 10-10-66-6	54.699699	-110.820299	632.6	1355.15	Loverna	metasedimentary	garnet-akali feldspar-biotite schist	Brecciated, foliated, crenulated, fine-grained, inequigranular, phaneritic, porphyroblastic	Foliated, brecciated, porphyroblastic, fine-grained garnet-alkali feldspar-biotite schist. Pervasive shattered to mosaic-healed brecciated texture that affects both matrix and porphyroblasts. Composed of subhedral platy biotite (up to 0.5 mm long), anhedral quartz (up to 0.5 mm), and anhedral alkali feldspar (0.5-1 mm). Breccia fractures filled by cryptocrystalline quartz or lesser opaque minerals. Garnet occurs as rare euhedral porphyroblasts (up to 5 mm) that are heavily fractured and locally filled by cryptocrystalline quartz or lesser calcite. Very fine grained chlorite is spatially associated with cryptocrystalline quartz.	33	-9999	27	-9999	-9999	-9999	30	5	-9999	3	-9999	-9999	-9999	-9999	1	1	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA048	drillcore	1AA/06-07-065-04W4/00	ESSO 80 LEPING OV 6-7-65-4	54.607881	-110.601376	627.2	1332.93	Loverna	gneiss	biotite-alkali feldspar gneiss	Foliated, banded, fine-grained, equigranular, phaneritic, granophyric	Foliated, banded, fine-grained biotite-alkali feldspar gneiss. Composed primarily of anhedral quartz and alkali feldspar with minor plagioclase (0.2-0.5 mm). Platy subhedral biotite (up to 1 mm long). Rare patches of calcite alteration replacing some grains and filling fractures.	40	2	33	-9999	-9999	-9999	24	-9999	-9999	-9999	-9999	-9999	-9999	-9999	1	-9999	tr	tr	tr	-9999	-9999	Alberta Geological Survey
24BA049	drillcore	100/01-32-064-03W4/00	ESSO 83 SWD ETHELLK 1-32-64-3	54.575268	-110.413196	660.0	1332.26	Loverna	gneiss	biotite gneiss	Banded, medium-grained, equigranular, phaneritic	Banded, medium-grained biotite gneiss. Primarily composed of subhedral, stubby plagioclase and anhedral quartz (1-3 mm) with minor anhedral alkali feldspar (0.25-0.5 mm). Lesser, subhedral, platy biotite (up to 1.5 mm long).	37	47	2	-9999	-9999	-9999	10	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	2	tr	tr	tr	-9999	-9999	Alberta Geological Survey
24BA050	drillcore	100/01-32-064-03W4/00	ESSO 83 SWD ETHELLK 1-32-64-3	54.575268	-110.413196	660.0	1335.56	Loverna	gneiss	biotite gneiss	Banded, medium-grained, equigranular, phaneritic	Banded, medium-grained biotite gneiss. Primarily composed of anhedral quartz and subhedral plagioclase (1-3 mm) with lesser anhedral alkali feldspar (0.25-0.5 mm). Feldspars are weakly altered to very fine grained sericite. Biotite as platy aggregates (up to 1.5 mm long).	39	47	2	-9999	-9999	-9999	10	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	1	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA051	drillcore	100/02-02-073-01W6/00	Canlin PUSKWA 2-2-73-1	55.289031	-118.035585	677.6	3102.92	Chinchaga	metavolcanic	chlorite schist	Foliated, moderately altered, fine-grained, inequigranular, phaneritic	Foliated, fine-grained chlorite schist. Primarily composed of anhedral quartz (0.2-2 mm) and relict feldspar altered completely to sericite (up to 3 mm). Pervasive, moderate alteration, particularly alteration of feldspars to sericite. Foliation parallel, platy chlorite (up to 0.5 mm long) as aggregates and bands. Chlorite spatially associated with equant opaque minerals and patches of very fine grained epidote with ragged margins.	25	-9999	15	-9999	-9999	-9999	-9999	-9999	38	15	2	-9999	-9999	-9999	-9999	5	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA053	drillcore	100/02-02-073-01W6/00	Canlin PUSKWA 2-2-73-1	55.289031	-118.035585	677.6	3105.25	Chinchaga	metavolcanic	chlorite schist	Foliated, moderately altered, fine-grained, inequigranular, phaneritic	Foliated, fine-grained chlorite schist. Primarily composed of anhedral quartz (0.2-1 mm) and relict feldspar altered completely to sericite (up to 2 mm). Pervasive, moderate alteration, particularly alteration of feldspars to sericite. Foliation parallel, platy chlorite (up to 0.5 mm long) as aggregates and bands. Chlorite spatially associated with equant opaque minerals and patches of very fine grained epidote with ragged margins. Quartz veins (up to 1 cm) composed primarily of quartz (up to 3 mm) and minor chlorite.	30	-9999	10	-9999	-9999	-9999	-9999	-9999	38	15	2	-9999	-9999	-9999	-9999	5	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA054	drillcore	100/06-05-055-17W4/00	WHITECAP WILDON 6-5-55-17	53.722681	-112.495674	676.0	2118.59	Lacombe	metavolcanic	muscovite-chlorite-biotite schist	Foliated, fine-grained, inequigranular, aphanitic	Foliated, fine-grained muscovite-chlorite-biotite schist. Primarily composed of microcrystalline anhedral quartz (50-75 m) with occasional quartz phenocrysts (up to 1 mm). Matrix also contains very fine grained biotite, chlorite, and muscovite that are aligned to foliation. Occasional foliation-parallel vugs rimmed by opaque minerals.	60	-9999	-9999	-9999	-9999	-9999	14	-9999	12	12	-9999	-9999	-9999	-9999	-9999	2	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA055	drillcore	100/06-05-055-17W4/00	WHITECAP WILDON 6-5-55-17	53.722681	-112.495674	676.0	2120.97	Lacombe	metavolcanic	muscovite-biotite-chlorite schist	Foliated, fine-grained, aphanitic, inequigranular	Foliated, fine-grained muscovite-biotite-chlorite schist. Primarily composed of microcrystalline anhedral quartz (50-150 m) with occasional quartz phenocrysts and aggregates (up to 1 mm). Matrix also contains very fine grained biotite, chlorite, and muscovite that are aligned to foliation. Disseminated, very fine grained opaque minerals.	55	-9999	-9999	-9999	-9999	-9999	14	-9999	11	18	-9999	-9999	-9999	-9999	-9999	2	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA056	drillcore	100/02-29-085-09W4/00	SUNCOR ET AL HANGSTN 2-29-85-9	56.393732	-111.386687	567.3	727.97	Taltson Charles Lake - Athabasca	granitoid	biotite granite	Foliated, lineated, medium- to coarse-grained, inequigranular, phaneritic, granophyric	Strained, foliated, medium- to coarse-grained biotite granite. Phenocrysts of stubby to tabular, anhedral alkali feldspar (up to 1 cm) and plagioclase (up to 5 mm) set in a matrix of feldspar, quartz, and biotite. Aggregates of recrystallized and stretched, anhedral quartz (0.2-1 mm). Feldspar and quartz often form granophyric textures. Foliation-aligned, platy biotite with lesser muscovite (up to 1 mm). Weak alteration of feldspar to sericite. Occasional, anhedral, interstitial patches of opaque minerals, often aligned with foliation.	30	15	40	-9999	-9999	-9999	10	-9999	2	-9999	-9999	-9999	-9999	-9999	-9999	3	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA057	drillcore	100/02-29-085-09W4/00	SUNCOR ET AL HANGSTN 2-29-85-9	56.393732	-111.386687	567.3	728.49	Taltson Charles Lake - Athabasca	granitoid	biotite granite	Foliated, lineated, medium- to coarse-grained, inequigranular, phaneritic, granophyric	Weakly altered, strained, medium- to coarse-grained biotite granite. Phenocrysts of stubby to tabular, anhedral alkali feldspar (up to 1 cm) and plagioclase (up to 4 mm) set in a matrix of feldspar, quartz, and biotite. Aggregates of recrystallized and stretched, anhedral quartz (0.2-2 mm). Feldspar and quartz often form granophyric textures. Foliation-aligned, platy biotite with lesser muscovite (up to 1 mm). Weak alteration of feldspar to sericite. Biotite altered to chlorite with ragged margins and spatially associated with opaque minerals. Occasional, anhedral, interstitial patches of opaque minerals, often aligned with foliation.	33	12	40	-9999	-9999	-9999	7	-9999	2	3	-9999	-9999	-9999	-9999	tr	3	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA059	drillcore	111/07-31-094-05W4/00	SUNCOR OB191 FIREBAG 7-31-94-5	57.197448	-110.794260	583.2	421.12	Taltson Charles Lake - Athabasca	granitoid	biotite granite	Fine- to medium-grained, inequigranular, phaneritic, granophyric	Fine- to medium-grained biotite granite. Primarily composed of quartz (0.2-2 mm), plagioclase (0.5-4 mm), and lesser alkali feldspar (0.5-2 mm). Feldspar crystals are weakly altered to sericite. Platy, subhedral biotite (up to 1 mm long) is locally altered to chlorite. Opaque minerals fill thin (<1 mm), discontinuous fractures and form interstitial texture around crystals.	39	32	14	-9999	-9999	-9999	7	-9999	3	3	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA060	drillcore	111/07-31-094-05W4/00	SUNCOR OB191 FIREBAG 7-31-94-5	57.197448	-110.794260	583.2	424.75	Taltson Charles Lake - Athabasca	granitoid	granite	Medium-grained, inequigranular, phaneritic, granophyric	Medium-grained granite. Primarily composed of anhedral quartz, plagioclase, and alkali feldspar (0.5-4 mm). Occasional granophyric texture from intergrowths of quartz and feldspar crystals. Embayed biotite (up to 1.5 mm long), often altered chlorite with ragged margins. Feldspar crystals are often altered to sericite which forms in parallel bands and the cores of feldspars. Rare patches of calcite alteration. Occasional, equant to interstitial opaque minerals.	40	27	23	-9999	-9999	-9999	4	-9999	2	3	-9999	-9999	-9999	-9999	tr	1	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA061	drillcore	100/01-27-060-26W4/00	IMP-BAYSEL RIVERDALE NO. 1-27-60-26	54.212254	-113.803762	650.1	2291.34	Thorsby	granitoid	garnet granite	Fine- to medium-grained, inequigranular, phaneritic	Fine- to medium-grained garnet granite. Primarily composed of anhedral, recrystallized and stretched quartz (0.1-1 mm), anhedral, stubby to tabular alkali feldspar (0.2-5 mm), and anhedral, stubby to tabular plagioclase (0.2-5 mm). Feldspars partially altered to very fine grained sericite. Minor biotite is partially to completely replaced by chlorite with ragged margins. Occasional garnet (up to 1 mm) is heavily fractured and contains interstitial chlorite. 	40	21	35	-9999	-9999	-9999	tr	2	1	1	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA062	drillcore	100/15-24-109-17W5/00	IMPERIAL SURETTE LAKE NO. 1	58.483779	-116.690304	309.4	1361.30	Buffalo High	granitoid	granite	Moderately altered, medium- to coarse-grained, inequigranular, phaneritic	Moderately altered, medium- to coarse-grained granite. Primarily composed of deformed, subhedral to euhedral plagioclase (0.5-10 mm) with lesser subhedral to euhedral alkali feldspar (0.5-10 mm) and recrystallized, anhedral quartz (0.5-10 mm). Embayed, anhedral amphibole with inclusions of apatite, opaque minerals, and chlorite. Abundant epidote crystals (up to 2 mm), spatially associated with equant to interstitial opaque minerals and lesser fine-grained chlorite.	16	37	21	-9999	-9999	5	-9999	-9999	tr	1	12	-9999	-9999	-9999	-9999	7	tr	-9999	1	-9999	-9999	Alberta Geological Survey
24BA063	drillcore	100/07-34-083-15W5/00	ALBERTA856 SLAVE 7-34-83-15	56.235621	-116.276591	698.1	1783.35	Buffalo High	granitoid	biotite alkali feldspar granite	Medium-grained, inequigranular, phaneritic	Medium-grained biotite alkali feldspar granite. Primarily composed of stubby, subhedral alkali feldspar (0.5-5 mm) and anhedral quartz (0.3-2 mm). Common aggregates (up to 5 mm wide) of cryptocrystalline quartz and sericite form an interstitial fabric between grains and locally replace relict grains of unknown mineralogy. Abundant, platy biotite (up to 1 mm long), commonly partially replaced by chlorite. Disseminated, subhedral to euhedral, equant to tabular opaque minerals. Occasional patches of calcite alteration.	35	-9999	40	-9999	-9999	-9999	15	-9999	3	2	-9999	-9999	-9999	-9999	tr	5	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA064	drillcore	100/12-30-125-02W6/00	SHELL THURSTON LAKE 30-125-2	59.889970	-118.345366	745.8	1826.11	Great Bear	granitoid	granite	Medium-grained, inequigranular, phaneritic	Moderately altered, medium-grained granite. Primarily composed of anhedral quartz (0.2-4 mm), stubby anhedral alkali feldspar (0.3-3 mm) and stubby anhedral plagioclase (0.3-3 mm). Plagioclase is partially to completely replaced by sericite. Biotite occurs as "books" and is replaced by chlorite with ragged margins. Occasional, subhedral, equant opaque minerals (up to 0.5 mm).	38	10	28	-9999	-9999	-9999	2	-9999	10	10	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA065	drillcore	100/14-20-095-06W5/00	BSRL PANNY 14-20-95-6	57.261794	-114.936229	538.1	1237.10	Buffalo Utikuma	metasedimentary	sillimanite-garnet-cordierite-biotite granofels	Granoblastic, fine-grained, inequigranular, phaneritic	Fine-grained sillimanite-garnet-cordierite-biotite granofels. Primarily composed of recrystallized, granoblastic, anhedral quartz (0.1-2 mm). Lesser anhedral alkali feldspar and plagioclase (0.1-0.5 mm). Disseminated, platy, anhedral biotite (0.1-0.5 mm) and disseminated, equant, subhedral opaque minerals (up to 0.5 mm). Minor amounts of embayed garnet (up to 0.5 mm) along with fine-grained masses of sillimanite, embayed, pinitized cordierite, and platy, very fine grained muscovite.	80	5	5	-9999	-9999	-9999	5	1	tr	-9999	-9999	1	1	-9999	-9999	2	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA066	drillcore	100/14-20-095-06W5/00	BSRL PANNY 14-20-95-6	57.261794	-114.936229	538.1	1239.17	Buffalo Utikuma	metasedimentary	sillimanite-biotite-garnet granofels	Granoblastic, fine-grained, inequigranular, phaneritic	Fine-grained sillimanite-biotite-garnet granofels. Mainly composed of recrystallized, granoblastic quartz (0.1-2 mm). Lesser anhedral alkali feldspar and plagioclase (0.2-1 mm). Disseminated subhedral, equant opaque minerals (up to 0.5 mm) and anhedral, platy biotite (up to 0.5 mm). Embayed, equant, subhedral garnet (up to 1 mm) with numerous inclusions. Lesser masses of acicular, very fine grained acicular sillimanite. A single very fine grained to cryptocrystalline biotite-garnet-opaque minerals-quartz wide vein (1 mm wide).	55	10	20	-9999	-9999	-9999	3	4	-9999	-9999	-9999	1	-9999	-9999	-9999	7	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA067	drillcore	100/06-10-077-25W4/00	IMP PELICAN HILLS 6-10-77-25	55.655195	-113.799995	797.4	1861.67	Unknown	gneiss	garnet-cordierite gneiss	Granoblastic, fine- to medium-grained, inequigranular, phaneritic	Fine- to medium-grained garnet-cordierite gneiss. Primarily composed of anhedral, stretched quartz (0.1-3 mm) with lesser anhedral alkali feldspar (0.1-1 mm) and plagioclase (0.1-0.5 mm). Pinitized cordierite (up to 3 mm) spatially associated with fractured garnet (up to 2 mm). Lesser, disseminated opaque minerals and patches of sericite alteration.	45	5	15	-9999	-9999	-9999	-9999	10	2	-9999	-9999	-9999	18	-9999	-9999	5	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA068	drillcore	100/06-10-077-25W4/00	IMP PELICAN HILLS 6-10-77-25	55.655195	-113.799995	797.4	1863.86	Unknown	gneiss	biotite-cordierite-garnet gneiss	Medium-grained, inequigranular, phaneritic	Medium-grained biotite-cordierite-garnet gneiss. Primarily composed of anhedral quartz (0.2-7 mm) and lesser plagioclase (0.2-2 mm). Subhedral, fractured garnet (up to 3 mm), spatially associated with embayed, pinitized cordierite and platy, subhedral biotite. Lesser subhedral to anhedral, equant to interstitial opaque minerals.	60	20	-9999	-9999	-9999	-9999	2	8	1	-9999	-9999	-9999	7	-9999	-9999	2	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA069	drillcore	100/10-20-062-08W5/00	MOBIL OIL GOOSE CREEK 10-20-62-8	54.379380	-115.160574	776.6	2786.65	Wabamun	granitoid	biotite granite	Foliated, moderately altered, fine- to medium-grained, inequigranular, phaneritic	Foliated, moderately altered, fine-  to medium-grained biotite granite. Primarily composed of anhedral quartz (0.2-2 mm), anhedral to subhedral alkali feldspar (0.2-2 mm), and lesser anhedral to subhedral plagioclase (0.2-4 mm). Platy, subhedral biotite (up to 0.5 mm long) aligned to foliation and weakly altered to chlorite. Feldspars altered to sericite. Minor calcite fills interstitial spaces and replaces grains.	41	14	28	-9999	-9999	-9999	9	-9999	5	1	-9999	-9999	-9999	-9999	2	tr	tr	-9999	tr	-9999	-9999	Alberta Geological Survey
24BA070	drillcore	100/15-27-077-12W5/02	CPEC LHORSE 1-34-77-12	55.711554	-115.764643	712.9	2138.29	Buffalo High	gneiss	amphibole-biotite gneiss	Banded, foliated, moderately altered, fine-grained, inequigranular, phaneritic	Banded, foliated, moderately altered, fine-grained amphibole-biotite gneiss. Leucosomes composed of anhedral quartz (0.1-1.5 mm), anhedral alkali feldspar (0.1-0.5 mm), and stubby, subhedral plagioclase (0.1-2 mm). Melanosomes composed of tabular, subhedral to anhedral hornblende (up to 1 mm long) and platy, subhedral biotite (up to 1 mm long). Disseminated aggregates of very fine grained clusters of epidote with ragged margins. Feldspar altered to very fine grained sericite and biotite altered to very fine grained chlorite. Minor amounts of euhedral to subhedral titanite (up to 0.3 mm).	30	28	22	-9999	-9999	5	9	-9999	1	1	2	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	2	Alberta Geological Survey
24BA072	drillcore	100/05-35-062-18W5/00	CHEVRON GULF FOX CK 5-35-62-18	54.404769	-116.598318	877.2	3448.00	Chinchaga	amphibolite	amphibolite	Weakly foliated, moderately altered, fine- to medium-grained, inequigranular, phaneritic	Weakly foliated, fine- to medium-grained amphibolite. Primarily composed of subhedral, tabular amphibole (up to 5 mm) and anhedral plagioclase (up to 1 mm). Lesser relict pyroxene (up to 1 mm) altered to very fine grained calcite, chlorite, and epidote. Minor amounts of equant, subhedral opaque minerals (up to 0.5 mm).	-9999	40	-9999	-9999	-9999	40	-9999	-9999	-9999	5	4	-9999	-9999	-9999	9	2	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA073	drillcore	100/08-16-088-02W6/00	CLEAR HILLS NO. 8-16	56.629742	-118.242491	731.8	2103.62	Unknown	granitoid	granite	Fine-grained, porphyritic, inequigranular, phaneritic	Fine-grained granite. Primarily composed of anhedral quartz (0.5-1 mm), anhedral to subhedral alkali feldspar (approximately 0.5 mm), and lesser anhedral plagioclase (approximately 0.5 mm). Phenocrysts of stubby, subhedral alkali feldspar (up to 3 mm). Minor patches of fine-grained chlorite with ragged margins. Weak calcite alteration replacing occasional crystals.	50	20	25	-9999	-9999	-9999	-9999	-9999	-9999	4	-9999	-9999	-9999	-9999	1	tr	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA074	drillcore	100/07-14-057-06W4/00	TEXEX ET AL ELK POINT 7-14-57-6	53.924261	-110.781760	604.7	1588.38	Loverna	gneiss	biotite gneiss	Banded, moderately foliated, fine-grained, inequigranular, phaneritic	Moderately foliated, banded (1 cm), fine-grained biotite gneiss. Leucosomes are primarily composed of anhedral alkali feldspar (0.2-3 mm), anhedral quartz (0.2-1 mm), and lesser, anhedral plagioclase (approximately 0.5 mm). Plagioclase is commonly partitioned into different leucosomes than alkali feldspar. Melanosomes composed of platy, embayed, subhedral biotite (up to 1 mm), locally altered to chlorite. Feldspar, particularly plagioclase, partially altered to very fine grained sericite. Occasional, thin calcite veinlets.	30	18	37	-9999	-9999	-9999	7	-9999	3	4	-9999	-9999	-9999	-9999	tr	1	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA076	drillcore	100/07-18-064-03W4/00	ESSO 79 SWD COLDLK 7-18-64-3	54.535581	-110.443813	587.2	1287.71	Loverna	gneiss	biotite gneiss	Banded, moderately foliated, fine- to medium-grained, inequigranular, phaneritic	Moderately foliated, fine- to medium-grained biotite gneiss. Primarily composed of anhedral to subhedral plagioclase (up to 5 mm) and stretched, anhedral quartz (0.2-3 mm). Platy, subhedral biotite (up to 1 mm long) and lesser, disseminated patches of opaque minerals. Feldspar altered to sericite and weak, patchy calcite alteration.	39	45	-9999	-9999	-9999	-9999	12	-9999	1	-9999	-9999	-9999	-9999	-9999	1	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA077	drillcore	100/10-15-038-21W4/00	CPOG OBERLIN 10-15-38-21	52.268384	-112.919227	819.6	2869.24	Lacombe	metavolcanic	biotite-muscovite schist	Intensely foliated, very fine grained, porphyritic, inequigranular, phaneritic	Intensely foliated, very fine grained biotite-muscovite schist. Intense foliation with augen textures and deformation bands. Primarily composed of very fine grained to cryptocrystalline quartz groundmass with lesser muscovite and biotite. Occasional stubby, subhedral plagioclase phenocrysts (up to 2 mm). Pervasive, very fine grained calcite alteration.	45	10	-9999	-9999	-9999	-9999	5	-9999	10	-9999	-9999	-9999	-9999	-9999	30	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA079	drillcore	100/11-08-075-22W5/00	TERRAQUEST MCLEANS CK 11-8-75-22	55.484276	-117.381663	589.2	2584.94	Chinchaga	granitoid	biotite alkali feldspar granite	Fractured, moderately foliated, fine- to medium-grained, porphyritic, inequigranular, phaneritic	Fractured, moderately foliated, fine- to medium-grained biotite alkali feldspar granite. Brittle deformation with fractured phenocrysts set in a very fine grained to cryptocrystalline matrix. Phenocrysts consist of anhedral quartz (up to 3 mm) and stubby, subhedral alkali feldspar (up to 2 mm) with minor platy, subhedral biotite (up to 1 mm long) that wraps around phenocryst margins. Matrix composed of very fine grained to cryptocrystalline quartz and sericite.	35	-9999	42	-9999	-9999	-9999	15	-9999	5	-9999	-9999	-9999	-9999	-9999	-9999	3	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA080	drillcore	100/11-08-075-22W5/00	TERRAQUEST MCLEANS CK 11-8-75-22	55.484276	-117.381663	589.2	2586.44	Chinchaga	granitoid	biotite granite	Medium-grained, inequigranular, phaneritic	Medium-grained biotite granite. Primarily composed of anhedral quartz and alkali feldspar (0.2-3 mm) with lesser stubby, subhedral plagioclase (0.2-5 mm). Disseminated, subhedral, platy biotite with weak alteration to chlorite. Feldspar locally altered to very fine grained sericite.	33	22	33	-9999	-9999	-9999	10	-9999	2	tr	-9999	-9999	-9999	-9999	-9999	-9999	tr	tr	-9999	-9999	-9999	Alberta Geological Survey
24BA081	drillcore	100/16-12-066-13W5/00	HOME UNION HB VIRGINIA HILLS 16-12	54.703171	-115.819177	1167.4	3203.87	Buffalo Arch	granitoid	tonalite	Medium-grained, inequigranular, phaneritic	Medium-grained tonalite. Primarily composed of subhedral plagioclase (0.3-4 mm) and anhedral quartz (0.2-3 mm). Relict biotite completely altered to fine-grained, anhedral chlorite with ragged margins and very fine grained aggregates of opaque minerals. Plagioclase partially altered to very fine grained sericite.	40	45	-9999	-9999	-9999	-9999	-9999	-9999	4	10	-9999	-9999	-9999	-9999	-9999	1	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
24BA082	drillcore	100/10-06-082-01W5/00	IMP. FUTURITY GODIN LAKE 10-6-82-1	56.081443	-114.141808	581.6	1526.64	Buffalo Utikuma	granitoid	tonalite	Coarse-grained, inequigranular, porphyritic, phaneritic	Coarse-grained plagioclase-phyric tonalite. Tabular, subhedral plagioclase (up to 1 cm long) set in a matrix of fine-grained, granoblastic quartz (approximately 0.5 mm). Lesser anhedral alkali feldspar (up to 2 mm). Anhedral, fine-grained biotite, commonly partially or completely altered to chlorite, locally rimming plagioclase phenocrysts. Plagioclase commonly weakly altered to very fine grained sericite.	50	40	5	-9999	-9999	-9999	2	-9999	2	1	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA001	drillcore	100/01-23-079-11W5/00	SUMMERLAND GIFT 1-23-79-11	55.855538	-115.593750	668.9	1833.33	Buffalo Utikuma	syenitoid	quartz syenite	Fine- to medium-grained, inequigranular, phaneritic	Fine- to medium-grained quartz syenite. Blocky, subhedral alkali feldspar (up to 10 mm) with lesser quartz and plagioclase (approximately 0.5-1 mm). Minor garnet (up to 2 mm), biotite, chlorite, and muscovite. Weak sericite alteration of feldspars and chlorite alteration of garnet. Cut by thin (sub-mm), sheared quartz veinlets.	17	23	55	-9999	-9999	-9999	1	1	2	1	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA002	drillcore	100/01-23-079-11W5/00	SUMMERLAND GIFT 1-23-79-11	55.855538	-115.593750	668.9	1837.51	Buffalo Utikuma	gneiss	biotite gneiss	Weakly foliated, weakly banded, fine-grained, equigranular, phaneritic	Weakly foliated and banded, fine-grained biotite gneiss. Mainly composed of quartz and feldspar (approximately 0.5 mm) with disseminated platy biotite (up to 1 mm long) and minor garnet (up to 1 mm). Occasional melanosomal bands up to 2 mm wide comprised of biotite and garnet.	44	35	-9999	-9999	-9999	-9999	20	1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA003	drillcore	100/04-12-015-27W4/00	CHEVRON PARKLAND 4-12-15-27	50.238968	-113.595302	1008.6	3603.01	Vulcan Low	metavolcanic	andesite	Weakly foliated, weakly banded, very fine grained, inequigranular, phaneritic	Weakly foliated, very fine grained to fine-grained andesite. Mainly composed of anhedral plagioclase (0.5-1 mm) with lesser anhedral quartz (approximately 0.5 mm). Disseminated biotite (up to 1 mm long) that sometimes forms aggregates. Minor garnet (up to 4 mm) and equant to botryoidal opaque minerals (up to 0.5 mm). Weak alteration of plagioclase to sericite and epidote.	20	50	-9999	-9999	-9999	-9999	25	2	1	-9999	tr	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA004	drillcore	100/05-31-065-06W5/00	HUDSON'S BAY EAST VIRGINIA HILLS 1	54.666747	-114.906106	797.1	2563.00	Buffalo Arch	gabbroid	biotite-hornblende quartz gabbro	Moderately altered, moderately foliated, fine- to medium-grained, inequigranular, phaneritic, porphyritic	Moderately foliated and altered, fine- to medium-grained biotite-hornblende quartz gabbro. Primarily composed of plagioclase (up to 2 mm in width), tabular hornblende (0.2-1.5 mm long), and platy biotite (up to 1.5 mm long). Amphibole may be replacing relict pyroxene. Patches of anhedral, stretched quartz. Moderate sericite and weak epidote alteration of plagioclase.	10	34	-9999	-9999	-9999	28	17	-9999	10	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA005	drillcore	102/05-35-059-21W4/00	SCL THORH 5-35-59-21	54.143162	-113.045751	646.8	2101.17	Rimbey	gneiss	amphibole-clinopyroxene gneiss	Banded, fine- to medium-grained, inequigranular, phaneritic	Banded, fine- to medium-grained amphibole-clinopyroxene gneiss. Banding is not resolvable at thin section scale. Primarily composed of subhedral, blocky plagioclase (0.5-3 mm) with lesser blocky clinopyroxene (0.5-2 mm) and blocky, embayed amphiboles (up to 2 mm). Disseminated, equant opaque minerals (0.5-2 mm). Plagioclase is altered to very fine grained, patchy sericite, occasionally entire grains are altered to sericite. Rare very fine grained patches of epidote and chlorite alteration.	-9999	65	-9999	-9999	14	10	-9999	-9999	6	1	2	-9999	-9999	-9999	-9999	2	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA006	drillcore	103/06-09-060-15W4/00	PEMBINA PIPELI ACG BELLIS 6-9-60-15	54.170917	-112.191427	681.1	1893.19	Loverna	granitoid	muscovite granite	Coarse-grained, inequigranular, phaneritic	Coarse-grained muscovite granite. Primarily composed of blocky, subhedral alkali feldspar (5-10 mm) with lesser anhedral quartz (0.5-5 mm) and anhedral, blocky plagioclase (0.5-1 mm). Primary aggregates of platy muscovite (up to 4 mm long). Weak alteration, including very fine grained sericite altering feldspars (primarily plagioclase), patches of calcite with ragged margins, and patches of very fine grained chlorite.	27	15	46	-9999	-9999	-9999	-9999	tr	10	1	-9999	-9999	-9999	-9999	1	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA007	drillcore	103/06-09-060-15W4/00	PEMBINA PIPELI ACG BELLIS 6-9-60-15	54.170917	-112.191427	681.1	1896.10	Loverna	granitoid	biotite tonalite	Fine- to medium-grained, equigranular, phaneritic	Fine- to medium-grained tonalite. Primarily composed of blocky to tabular, subhedral plagioclase (0.5-2 mm) and anhedral quartz (0.5-3 mm) with minor blocky, anhedral alkali feldspar (0.5-1 mm). Disseminated, platy biotite (up to 1.5 mm long). Weak alteration, including very fine grained sericite replacing plagioclase and patches of fine-grained calcite with ragged margins.	40	45	3	-9999	-9999	-9999	10	-9999	1	tr	-9999	-9999	-9999	-9999	1	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA008	drillcore	100/07-32-089-10W4/00	AOC GRANITE 7-32-89-10	56.759454	-111.554658	409.3	2352.32	Taltson Charles Lake - Athabasca	gneiss	quartzofeldspathic gneiss	Banded, fine-grained, equigranular, phaneritic	Banded, fine-grained quartzofeldspathic gneiss. Banding is not resolvable at this scale. Primarily composed of anhedral quartz (0.5-2 mm) with lesser anhedral alkali feldspar (0.5-2 mm) and plagioclase (0.5-2 mm). Clusters of equant orthopyroxene (up to 0.5 mm) and disseminated, equant opaque minerals (up to 0.5 mm). Minor disseminated, platy biotite (up to 0.5 mm long). Rare patches of calcite alteration with ragged margins.	50	15	30	3	-9999	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	tr	1	-9999	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA009	drillcore	100/07-32-089-10W4/00	AOC GRANITE 7-32-89-10	56.759454	-111.554658	409.3	2356.73	Taltson Charles Lake - Athabasca	gneiss	orthopyroxene gneiss	Banded, fine- to medium-grained, equigranular, phaneritic, myrmekitic	Banded, fine- to medium-grained orthopyroxene gneiss. Banding is not resolvable at this scale. Primarily composed of anhedral quartz (0.5-3 mm) with lesser anhedral plagioclase (0.5-2 mm) and alkali feldspar (0.5-2 mm). Clusters of equant orthopyroxene (up to 1 mm) and disseminated, equant opaque minerals (up to 1 mm). Minor disseminated, platy biotite (up to 0.5 mm long).	45	25	20	8	-9999	-9999	1	-9999	-9999	-9999	-9999	-9999	-9999	-9999	-9999	1	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA010	drillcore	100/07-32-089-10W4/00	AOC GRANITE 7-32-89-10	56.759454	-111.554658	409.3	2362.25	Taltson Charles Lake - Athabasca	gneiss	orthopyroxene gneiss	Banded, fine- to medium-grained, equigranular, phaneritic, myrmekitic	Banded, fine- to medium-grained orthopyroxene gneiss. Banding is not resolvable at this scale. Primarily composed of anhedral plagioclase (0.5-2 mm) quartz (0.5-3 mm) with lesser anhedral alkali feldspar (0.5-2 mm). Clusters of equant orthopyroxene (up to 1 mm) and disseminated, equant opaque minerals (up to 1 mm). Minor disseminated, platy biotite (up to 0.5 mm long). Trace very fine grained sericite and chlorite alteration.	35	40	10	10	-9999	-9999	3	-9999	tr	tr	-9999	-9999	-9999	-9999	-9999	2	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA011	drillcore	100/10-27-080-08W5/00	MOBIL NW NIPISI 10-27-80-8	55.965777	-115.159519	661.4	1844.80	Buffalo Utikuma	syenitoid	biotite quartz monzonite	Moderately altered, coarse-grained, inequigranular, phaneritic, porphyritic, myrmekitic	Moderately altered, coarse-grained biotite quartz monzonite. Phenocrysts of tabular, subhedral alkali feldspar (up to 10 mm). Finer-grained matrix composed of blocky, anhedral plagioclase (0.5-1 mm), platy biotite (up to 2 mm long), and minor anhedral quartz (0.5-1 mm). Relict clinopyroxene (up to 2 mm) is altered to very fine grained chlorite and sericite. Equant and interstitial opaque minerals (up to 1 mm). Trace alteration of plagioclase to fine-grained epidote with ragged margins.	5	27	35	-9999	5	-9999	10	-9999	3	10	tr	-9999	-9999	-9999	-9999	5	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA012	drillcore	100/12-29-081-09W5/00	SUMMERLAND NIPISI 12-29-81-9	56.053156	-115.379975	653.5	1729.47	Buffalo Utikuma	metavolcanic	felsic metavolcanic	Very fine grained, equigranular, aphanitic	Very fine grained felsic metavolcanic rock composed primarily of anhedral quartz, plagioclase, and alkali feldspar (0.35-0.5 mm). Disseminated clusters of very fine grained biotite, mainly altered chlorite. Disseminated opaque minerals (up to 0.3 mm).	35	35	20	-9999	-9999	-9999	1	-9999	-9999	8	-9999	-9999	-9999	-9999	-9999	1	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
25BA013	drillcore	100/16-18-107-06W6/00	IMPERIAL RAINBOW LAKE NO. 16-18-107-	58.296137	-118.980383	540.7	2242.41	Nova	gneiss	biotite gneiss	Banded, moderately foliated, moderately altered, fine- to medium-grained, equigranular, phaneritic	Moderately altered and foliated, fine- to medium-grained biotite gneiss. Irregular banding is 5-20 mm wide. Primarily composed of relict, blocky, subhedral plagioclase (1-2 mm), anhedral quartz (0.5-2 mm) and clusters of platy biotite (up to 2 mm long). Biotite is partially altered to chlorite and plagioclase is partially altered to sericite.	25	30	-9999	-9999	-9999	-9999	15	-9999	15	15	-9999	-9999	-9999	-9999	-9999	-9999	tr	-9999	-9999	-9999	-9999	Alberta Geological Survey
