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File Created: 14-Dec-2013 by Karl A. Flower (KAF)
Last Edit:  17-Dec-2013 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name K 11-12, K 11, K 12 Mining Division Alberni
BCGS Map 092E039
Status Showing NTS Map 092E08W
Latitude 049º 21' 32'' UTM 09 (NAD 83)
Longitude 126º 16' 29'' Northing 5470925
Easting 697886
Commodities Copper Deposit Types
Tectonic Belt Insular Terrane Wrangell, Plutonic Rocks
Capsule Geology

The K 11-12 occurrences are exposed from the shoreline facing Mate Island and for at least 600 metres inland.

The area is underlain by high-grade metamorphic volcanic rocks of the Paleozoic- Mesozoic Westcoast Complex (Geological Survey of Canada, Map 1537A). These have been intruded by diorite of the Eocene Catface Intrusions.

Locally, scattered outcrops of micro-diorite and gneissic diorite host chalcopyrite and magnetite mineralization. Grab samples of the outcrops yielded values from 0.011 to 0.098 per cent copper (Assessment Report 3750).

In 1972, Florex Mining completed a program of geological mapping, rock and soil sampling and a ground magnetic survey on the area as the K claims.

Bibliography
EMPR ASS RPT *3750
EMPR GEM 1972-261
GSC MAP 1537A
GSC OF 463
GSC P 53-17; 72-44; 80-16
Carson, D.J.T., (1968): Metallogenic Study of Vancouver Island with emphasis on the Relationship of Plutonic Rocks to Mineral Deposits, Ph.D. Thesis, Carleton University, Ottawa

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