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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  30-Oct-2014 by Laura deGroot (LDG)

Summary Help Help

NMI
Name IMPERIAL (L.9993), TATLER, WR, FARNHAM Mining Division Golden
BCGS Map 082K048
Status Prospect NTS Map 082K08W
Latitude 050º 25' 30'' UTM 11 (NAD 83)
Longitude 116º 28' 33'' Northing 5586017
Easting 537233
Commodities Copper, Silver Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Ancestral North America
Capsule Geology

The Imperial prospect is located at the headwaters of Farnham Creek, on the west flank of Black Diamond Mountain in the Golden Mining Division. The property consists of a single Reverted Crown grant (Lot 9993).

Regionally, the area is underlain by Proterozoic clastic sedimentary rocks of the Purcell and Windermere supergroups and by lower Paleozoic strata of the Beaverfoot and Mount Forster formations (Geoscience Map 1995-1).

The Purcell Supergroup strata include the Aldridge, Creston, Kitchener, Dutch Creek and Mount Nelson formations. The Windermere Supergroup unconformably overlies the Purcell Supergroup rocks and includes the Toby Formation and Horsethief Creek Group (Paper 1990-1).

In the vicinity of the occurrence, rocks of the Kitchener and Dutch Creek formations have been further subdivided and assigned to the Van Creek and Gateway formations. The Van Creek Formation correlates with the Lower Kitchener Formation while the Gateway Formation is equivalent to the lower portion of the Dutch Creek Formation. The Mount Nelson Formation has been subdivided into seven discrete members, a lower quartzite, a lower dolomite, a middle dolomite, a purple dolomite, an upper middle dolomite, an upper quartzite, and an upper dolomite (Open File 1990-26).

Rocks of the Horsethief Creek Group, Beaverfoot and Mount Forster formations are folded and overthrusted by rocks of the upper portion of the Dutch Creek Formation and the lower members of the Mount Nelson Formation. The sedimentary rocks have undergone regional metamorphism to at least greenschist facies.

The Imperial prospect consists of five quartz-barite veins containing some tetrahedrite and azurite. The main vein is 90 to 130 centimetres wide and has been exposed for approximately 30 metres along strike. The veins strike 155 degrees and dip 80 degrees west. All veins are within the middle dolomite member of the Mount Nelson Formation. Mineralization appears to be associated with tensional fractures on the crest of a northwest-trending anticline. A 1.22 metre wide chip sample across the main vein assayed 210 grams per tonne silver and 4.03 per cent copper (Assessment Report 21066).

Bibliography
EMPR AR 1920-114; 1926-448; 1968-266
EMPR ASS RPT 1614, 1977, 2515, 6099, 14574, *21066, 21789
EMPR EXPL 1976-E48; 1977-E66; 1985-C78
EMPR GEM 1969-343; 1970-469
EMPR GEOS MAP 1995-1
EMPR OF 1990-26, pp. 29-37
EMPR PF (82KSE General File - Geology map by P. Billingsley, 1958;
*see Copper King (082KSE003), Report on the Tatler Group by T.R.
Tough, 1967; *Sheppard, E.P. (1971): Geological Report on the
Tatler Group; Prospectors Report 1995-37 by Robert
Jordan)
GSC MAP 1957-12; 1326A
GSC MEM 148, p. 50; 369, p. 115
Pope, A.J. (1989): The Tectonics and Mineralization of the Toby-
Horsethief Creek Area, Purcell Mountains, Southeast British
Columbia, Canada, unpublished Ph.D. Thesis, University of London,
England
EMPR PFD 4137, 520084

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