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

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NMI
Name SYDNEY INLET MAGNETITE Mining Division Alberni
BCGS Map 092E049
Status Showing NTS Map 092E08W
Latitude 049º 26' 23'' UTM 09 (NAD 83)
Longitude 126º 15' 56'' Northing 5479934
Easting 698226
Commodities Iron, Magnetite Deposit Types
Tectonic Belt Insular Terrane Wrangell, Plutonic Rocks
Capsule Geology

The Sydney Inlet magnetite occurrence is located on the western shore of Sydney Inlet, approximately 700 metres south east of the entrance to Stewardson Inlet.

The area is underlain by granodioritic rocks of the Jurassic Island Plutonic Suite (Geological Survey of Canada Map 1537A).

Locally, a thin band of amphibolite striking south west is in contact with the intrusive rocks. The unit is approximately 200 metres wide and is part of the Paleozoic to Mesozoic West Coast Complex. The banded amphibolite is dark green to black in colour and consists of amphibole, plagioclase and magnetite. Selected samples assayed between 9.91 and 14.33 per cent iron (Assessment Report 462).

In 1962, Paco Resources completed a program of geological mapping on the area.

Bibliography
EMPR AR 1962-131
EMPR ASS RPT *462
GSC MAP 1537A
GSC OF 463
GSC P 71-36; 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
Sangster, D.F. (1964): The Contact Metosomatic Magnetite Deposits of Southwestern British Columbia, Ph.D. Thesis, University of British Columbia

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