British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  05-Jun-2023 by Karl A. Flower (KAF)

Summary Help Help

NMI 094C5 Mo1
Name GROUSE NORTH, GROUSE, ABE 8, ABE Mining Division Omineca
BCGS Map 094C031
Status Showing NTS Map 094C05W
Latitude 056º 20' 29'' UTM 10 (NAD 83)
Longitude 125º 48' 31'' Northing 6247619
Easting 326407
Commodities Molybdenum Deposit Types L04 : Porphyry Cu +/- Mo +/- Au
Tectonic Belt Intermontane Terrane Plutonic Rocks, Quesnel
Capsule Geology

The Grouse North molybdenum occurrence is located on the ridge north of the unnamed creek which drains into the west end of Tutizzi Lake, approximately 92 kilometres northwest of the community of Germansen Landing.

Regionally, the area is underlain by calc-alkaline and fine clastic sedimentary rocks of the Upper Triassic Takla Group that have been intruded by ultramafic and gabbroic to dioritic rocks of the Upper Triassic to Lower Jurassic Aiken Lake Intrusive Complex. Quartz monzonitic to monzogranitic intrusive rocks of the Lower Jurassic Hogem Plutonic Suite and monzodioritic to gabbroic intrusive rocks of the Mesilinka pluton are exposed to the southwest and south.

Assessment Report 3267 (page 3) states that very occasionally, molybdenite occurs in two well-developed fracture sets that strike northeast and north, dipping steeply. Barren white quartz veinlets are also common. Hostrocks are fine- to medium-grained, pink syenite of the Lower Jurassic to Lower Cretaceous Hogem Plutonic Suite. No other information is available.

Work History

The detection of a stream sediment geochemical anomaly in molybdenum led to the staking in September of 1970 of the Grouse 1-16 mineral claims. A soil sampling program was subsequently carried out over essentially the entire claim group by Union Miniere Explorations and Mining Corporation Limited.

During 1991 through 1994, Swannell Minerals Corp. completed programs of prospecting, geological mapping, geochemical (rock, silt and soil) sampling, a 13.1 line-kilometre ground magnetic survey, a 22.5 line-kilometre induced polarization survey and 10 diamond drillholes, totalling 897.9 metres, the area as the Abe 1-8 claims.

In 1998, Starfield Resources Inc. completed an extensive program of geological mapping, geochemical (rocks, silt and soil) sampling, a 35.8 line-kilometre ground magnetic and a 27.2 line-kilometre induced polarization survey on the Abe 1-8 and Norm 1-4 claims.

In 2004 and 2005, Commander Resources Ltd. completed programs of prospecting and geochemical (rock and soil) sampling on the Abe property. In 2007, Geoinformatics Exploration Canada Ltd. conducted a program of geological mapping, minor geochemical (rock and silt) sampling and five diamond drill holes, totalling 1600.0 metres, on the area as part of the regionally extensive Mesilinka property, which included the Abe property.

In 2012, on behalf of Commander Resources Ltd., a field program comprising reconnaissance prospecting, mapping and geochemical sampling was carried out on the Abe property. A total of 328 soil samples, 22 rock samples and 8 silt samples were collected and submitted for analysis.

During 2018 through 2021, Commander Resources Ltd. completed further programs of geological mapping and geochemical (rock and soil) sampling on the Omineca (Abe) property.

Bibliography
EMPR BULL 93
EMPR EXPL 1978-E241
EMPR FIELDWORK 1991, pp. 127-145; 1992, pp. 109-134; 2018, pp. 31-53; 2019, pp. 25-47
EMPR GEM 1971-60
EMPR GEOS MAP 2001-10
EMPR OF 1989-17; 1990-13; 1993-2; 1995-6; 1996-19
EMPR P 1992-01, pp. 127-145; 1993-01, pp. 109-134; 2019-01, pp. 31-53; 2020-01, pp. 25-47
GSC MAP 1030A
GSC MEM 274
GSC OF 864
GBC RPT 2021-01, pp. 105-120

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY