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File Created: 25-Mar-2020 by Karl A. Flower (KAF)
Last Edit:  19-Jul-2021 by George Owsiacki (GO)

Summary Help Help

NMI
Name CAS 3-9, LAKE 4 Mining Division Omineca
BCGS Map 094E006
Status Showing NTS Map 094E02W
Latitude 057º 03' 24'' UTM 09 (NAD 83)
Longitude 126º 54' 12'' Northing 6325647
Easting 627163
Commodities Silver Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Intermontane Terrane Stikine
Capsule Geology

The Cas 3-9 occurrence is located at an elevation of approximately 1180 metres on a southeast-trending ridge, approximately 600 metres west of Thutade Lake and 6 kilometres east-southeast of Thomas Peak, about 196 kilometres north-northwest of the community of Germansen Landing.

Regionally, the area is situated within a Mesozoic volcanic arc assemblage, which lies along the eastern margin of the Intermontane Belt, a northwest-trending belt of Paleozoic to Paleogene sediments, volcanics and intrusions bounded to the east by the Omineca Belt and to the west and southwest by the Sustut and Bowser basins. Devonian to Permian Asitka Group crystalline limestones are the oldest rocks exposed in the region. They are commonly in thrust contact with Upper Triassic Stuhini Group andesite flows, pyroclastic rocks and marine sedimentary rocks. The Asitka and Stuhini group rocks have been intruded by the Early Jurassic granodiorite to quartz monzonite Black Lake Suite and are in turn unconformably overlain by or faulted against Lower Jurassic calc-alkaline volcanics of the Toodoggone Formation (Hazelton Group). To the west these units are overlain by sedimentary rocks of the Middle to Upper Cretaceous Sustut Group.

The dominant structures in the area are steeply dipping faults that define a prominent regional northwest structural fabric trending 140 to 170 degrees. High angle, northeast-striking faults (approximately 060 degrees) appear to truncate and displace northwest-striking faults. Collectively these faults form a boundary for variably rotated and tilted blocks underlain by monoclinal strata.

Locally, a lapilli tuff hosts a multi-stage quartz vein with silver values. In 1992, a sample (4697) assayed 106 grams per tonne silver (Assessment Report 22721).

During 1984 through 1988, Pacific Ride Resources Corp. and Hermes Ventures Inc. examined the area as the Lake 4 claim. In 1991 and 1992, Placer Dome Inc. completed programs of rock and soil sampling, geological mapping and ground electromagnetic, magnetic and induced polarization surveys on the area as the Cas 3 and 6-9 claims.

Bibliography
EMPR ASS RPT 13025, 18241, 21944, *22721
EMPR BULL 86
EMPR EXPL 1975-E163-E167; 1976-E175-E177; 1977-E216-E217; 1978-E244-E246; 1979-265-267; 1980-421-436; 1982-330-345; 1983-475-488; 1984-348-357; 1985-C349-C362; 1986-C388-C414; 1987-C328-C346; 1988-C185-C194
EMPR FIELDWORK 1980, pp. 124-129; 1981, pp. 122-129, 135-141; 1982, pp. 125-127; 1983, pp. 137-138, 142-148; 1984, pp. 139-145, 291-293; 1985, pp. 167-169, 299; 1987, pp. 111, 114-115
EMPR GEM 1971-63-71; 1973-456-463
EMPR GEOLOGY 1977-1981, pp. 156-161
EMPR OF 2001-01
GSC BULL 270
GSC OF 306; 483
GSC P 80-1A, pp. 27-32
ECON GEOL Vol 86, pp. 529-554, 1991

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