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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  25-Apr-1988 by Laura L. Coughlan (LLC)

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NMI 104K14 Pb1
Name KING SALMON, KAP, KAP1-2, GOLDCAP, CAP 11, RED CAP Mining Division Atlin
BCGS Map 104K074
Status Showing NTS Map 104K14W
Latitude 058º 47' 00'' UTM 08 (NAD 83)
Longitude 133º 17' 53'' Northing 6517176
Easting 598388
Commodities Silver, Gold, Zinc, Lead, Copper Deposit Types
Tectonic Belt Intermontane Terrane Stikine, Plutonic Rocks
Capsule Geology

The property is situated between the Atlin Horst to the northeast and the Stikine Arch to the south. To the west, most units are under- lain by the granitic rocks of the Coast Plutonic Complex. These rocks have not been regionally metamorphosed or intensely folded as are the older units within the Tulsequah area.

The property is situated in the Upper Triassic Stuhini Group, King Salmon Formation, which is a northwest trending sequence of sedi- mentary and pyroclastic units. The formation occurs in a southeast plunging anticline that has been intruded by felsic dykes, which also trend in a northwest direction. The mineral occurrence was first discovered in 1980 by diamond drilling (Assessment Report 9246). Drill holes on the property intersected mineralized tuffs and brecciated tuffs. One drill hole encountered a 6.1-metre intercept grading 57.94 grams per tonne silver, 0.82 grams per tonne gold, 1.08 per cent zinc, 0.84 per cent lead, and 0.06 per cent copper (Basaba Enterprises, (1987)). Sericitized feldspar porphyry dykes intrude the King Salmon rocks, and are possibly of Late Cretaceous or Early Tertiary Age.

Sulphide mineralization in brecciated tuff consists of fine- grained pyrite and arsenopyrite disseminated in the quartz-rich matrix of the breccia. A 5.7-metre thick zone of massive sulphides was also encountered and contained massive, fine-grained arsenopyrite and some coarse-grained sphalerite in addition to finely banded arsenopyrite. Quartz and carbonate veins are common and some host pyrite and arseno- pyrite.

Argillic and carbonate alteration types are present as well as chalcedonic silica. Sulphides include disseminations of pyrite and arsenopyrite with stratiform lenses of pyrite, arsenopyrite, chalco- pyrite, galena, and sphalerite. The maximum observed widths of sulphide lenses was 20 centimetres.

In 1986, a grab sample of fine-grained grey sulphides within a stratiform rusty zone hosted by sandstone assayed 3.35 grams per tonne gold, 13.6 grams per tonne silver, 0.0195 per cent zinc, 0.0367 per cent lead, 0.0795 per cent copper, and 0.28 per cent arsenic (Assessment Report 15895).

Bibliography
EM EXPL 1999-19-31
EMPR ASS RPT *9246, 11421, *15895
EMPR EXPL 1982-398; 1983-547
EMPR PF (*Prospectus, Basaba Enterprises Inc., Aug.15, 1987: Report by Wahl, H. (1987), Kap-1 and Kap-2 Mineral Claims, Atlin Mining Division, B.C.)
GSC MAP 6-1960; 931A; 1262A
GSC MEM 248; *362
GSC P 45-30
GCNL #12,Jan.20, 1981
N MINER Jan.29, 1981
EMPR PFD 19946

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