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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  13-Aug-1988 by Laura L. Duffett (LLD)

Summary Help Help

NMI 093L14 Ag12
Name EMPIRE, RACHEL, BV, SUNSET, CASCADE Mining Division Omineca
BCGS Map 093L074
Status Past Producer NTS Map 093L14E, 093L14W
Latitude 054º 47' 00'' UTM 09 (NAD 83)
Longitude 127º 16' 56'' Northing 6072034
Easting 610470
Commodities Silver, Lead, Zinc, Gold, Copper, Cadmium, Antimony Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Intermontane Terrane Stikine
Capsule Geology

The claim is underlain by Lower to Middle Jurassic Hazelton Group volcanics comprised of andesitic flows, tuffs, and breccia. On the south side of the basin a shear, between 1443 to 1555 metres in elevation, hosts a mineralized quartz vein and is referred to as Empire #1. A selected high grade sample of galena and sphalerite from the 30 centimetre wide quartz vein assayed 2.05 grams per tonne gold, 7096 grams per tonne silver, 25.3 per cent lead, and 18.6 per cent zinc (1914) (Minister of Mines Annual Report 1914, page 225).

At elevation 1443 metres, an adit was driven along the shear which consisted of a 90 to 120 centimetre altered fracture zone with a well mineralized 8 to 30 centimetre quartz-sulphide vein with gouge along the footwall. The fracture eventually pinches out and reappears on the hanging wall to the south. The shear vein continues with little fracturing and consists of galena, sphalerite, arseno- pyrite with minor chalcopyrite, and tetrahedrite. In 1986, five chip samples were collected and assayed 0.6 to 3.3 grams per tonne gold, 57.9 to 1450 grams per tonne silver, 0.32 to 9.74 per cent lead, 0.22 to 8.47 per cent zinc with minor copper and cadmium values (Assessment Report 15140).

The Empire #1 shear vein is hosted in hornfelsed, fine-grained maroon to grey tuff. Recessive weathering shows the zone to be 30 metres wide and striking 160 degrees and dipping 80 degrees west. Manganese staining is common.

In 1914, three tonnes of ore was shipped from the Empire #1 workings and produced 20,030 grams silver and 699 kilograms lead.

On the northwest side of the basin, a mineralized vein referred to as Empire #2, strikes 310 degrees and dips 50 degrees west. The vein consists of 8 to 30 centimetres of silicified wall rock with quartz and abundant pyrite-galena-sphalerite and arsenopyrite. In 1986, three chip samples were taken across the vein as well as a high grade sample from the dump and assays ranged between 1.03 to 4.46 grams per tonne gold, 213.9 to 1292 grams per tonne silver, 7.5 to 36.67 per cent lead, 10.49 to 34.01 per cent zinc, 0.26 to 0.36 per cent copper, 0.07 to 0.23 per cent cadmium, and 0.02 to 0.12 per cent antimony (Assessment Report 15140).

Bibliography
EMPR AR 1909-84; 1912-115; 1914-225; 1920-90; 1921-272; 1924-96 1925-137; 1926-132; 1928-161; 1929-164; 1931-73; 1938-B37,C49; 1952-94; 1968-120,121
EMPR GEM 1969-85; 1971-177
EMPR MAP 69-1
EMPR EXPL *1986-359
EMPR ASS RPT *15140
EMPR FIELDWORK 1988, pp. 195-208; 1991, pp. 93-101
GSC MEM 223 (Rev) p. 93
GSC SUM RPT 1925A, p. 136
GSC MAP 278A; 971A
GSC P 44-23
GSC BULL 270
EMR MP CORPFILE (Buval Exec. Mining Ind. Ltd.; Abaca Resources Ind. Inc.)
W MINER Dec. 1952, p. 45
Kirkham, R.V., (1969): A Mineralogical and Geochemical Study of the Zonal Distribution of Ores in the Hudson Bay Range, British Columbia, Ph.D. Thesis, University of Wisconsin

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