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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  06-Nov-2009 by Kirk Hancock (KDH)

Summary Help Help

NMI
Name COMIN THROU BEAR, DEB, TARN Mining Division Cariboo
BCGS Map 093A085
Status Showing NTS Map 093A14E
Latitude 052º 53' 10'' UTM 10 (NAD 83)
Longitude 121º 04' 05'' Northing 5861349
Easting 629988
Commodities Lead, Zinc, Silver, Barite Deposit Types E12 : Mississippi Valley-type Pb-Zn
I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Cariboo
Capsule Geology

The occurrence is located near the headwaters of Kimball Creek at Black Stuart Mountain, 36 kilometres southeast of Barkerville or 43 kilometres northeast of Likely. Access to the property is by helicopter by 12 kilometres of horse-trail from the Matthew River logging camp northeast of Maeford Lake.

The region is underlain by rocks of the Cariboo Terrane which, in this area comprises formations of both the Cambrian-Mississippian Black Stuart Group and Upper Proterozoic-Cambrian Cariboo Group. Lithologies include dolostone breccia, clastic dolostone and limestone of the Mural Formation (Cariboo Group), and chert breccia and slate of the Black Stuart Group.

Showings occur at a number of locations on the property. Two types of mineralization have been identified but both types occur within a dolostone breccia. One type has galena associated with barite and is considered to be of sedimentary or diagenetic origin. The other type has galena, sphalerite and possibly tetrahedrite occurring as space fillings in brecciated quartz veining at the 'Tarn' showing with no obvious structural control on the localization of the veins. These quartz veins are restricted to the upper chert-dolostone breccia unit of the Mural Formation.

Bryan Elliott and Heather Scudder staked the "Comin Throu Bear" property in 1979 to cover an area of stream sediment zinc anomalies around Black Stuart Mountain. Teck Explorations Ltd. optioned the property in 1980 and performed geological and geochemical surveys which found stratiform lead-zinc-silver-barite mineralization in limestone of the Mural Formation. In 1980, the area was explored as part of Gulf Minerals Canada’s Cordilleran Sediments Geochemical Stream Sediment program. Two samples taken at this time near the head of Kimball Creek returned anomalous values in zinc and lead. In 1981, Teck Explorations Ltd. conducted geochemical, geological and drilling work which included 1522 soils, 53 silts, 1 water and 10 rock samples, geological mapping, and 16 diamond-drill holes totalling 465.6 metres of IAX core size. The Ter and Lin group of claims was staked in November, 1989 by Dual Resources Ltd, and in 1990 an airborne magnetometer and VLF-EM survey was completed over the entire property.

Bibliography
EMPR ASS RPT *8582, *9819, 21119
EMPR BULL 47
EMPR EXPL 1980-312, 1981-127
EMPR OF 1987-9; 1989-14, 20; 1990-31; 2001-11
EMPR P 1990-3
EMPR PF Chevron (Dillon, E.P. (1980-01-11): Cordilleran Sediments, Geochemical Stream Sediment Program, Quesnel Lake - Barkerville Area)
GSC MAP 12-1959; 1424A; 1538G
GSC OF 574; 844
NW PROSPECTOR Winter, 1985

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