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File Created: 10-May-2021 by George Owsiacki (GO)
Last Edit:  03-Mar-2023 by Larry Jones (LDJ)

Summary Help Help

NMI
Name 18 DMI-8-10, OS Mining Division Omineca
BCGS Map 094C012
Status Showing NTS Map 094C04W
Latitude 056º 10' 45'' UTM 10 (NAD 83)
Longitude 125º 47' 23'' Northing 6229511
Easting 326835
Commodities Copper, Silver Deposit Types L03 : Alkalic porphyry Cu-Au
Tectonic Belt Intermontane Terrane Plutonic Rocks, Quesnel
Capsule Geology

The 18 DMI-8-10 occurrence is located approximately 11 kilometres northeast of Ferriston Peak, 16 kilometres west of Tenakihi Peak, about 80 kilometres northwest of the community of Germansen Landing.

The showing is underlain by Thane Creek suite diorite in the Early Jurassic to Early Cretaceous Hogem Plutonic Suite in Quesnel terrane. The Thane Creek suite is mostly diorite to quartz monzodiorite, with lesser hornblendite.

Mineralization is inferred to be disseminated chalcopyrite in diorite. In 2018, a grab sample (18DMI-8-10) yielded assay results of 3860 parts per million copper, 10 parts per billion gold, and 3.3 parts per million silver (Fieldwork 2018, page 48).

The showing was mapped by the British Columbia Geological Survey during a regional bedrock mapping program in the Hogem batholith in 2018.

The area was explored as the OS Property by Cyprus Gold (Canada) Ltd. in 1990.

Bibliography
EMPR ASS RPT 21425
EMPR FIELDWORK 1991, pp. 127-145; 1992, pp. 109-134; *2018, pp. 31-53; 2019, pp. 25-47
EMPR P 1992-01, pp. 127-145; 1993-01, pp. 109-134; 2019-01, pp. 31-53; 2020-01, pp. 25-47
EMPR BULL 70
EMPR OF 2019-02; 2020-02
EMPR PRELIM MAP 9
GSC MAP 907A; 962A; 1030A
GSC MEM 274
GSC P 46-11; 48-5; 76-1A, pp. 69-73
Woodsworth, G.J., Anderson, R.G., and Armstrong, R.L. (1991): Plutonic regimes, Chapter 15. In: Gabrielse, H., and Yorath, C.J., (Eds.), Geology of the Cordilleran Orogen in Canada, Geological Survey of Canada, Geology of Canada, no. 4, pp. 491-531

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