Structural evolution of the Mitchell Au-Cu-Ag-Mo porphyry deposit, northwestern British Columbia
The Mitchell Au-Cu-Ag-Mo porphyry deposit, hosted by Early Jurassic volcanosedimentary and intrusive rocks in the Stikine terrane of northwestern British Columbia, is considered the largest undeveloped gold resource in Canada. As of 2015 it held a resource of 1777 Mt at 0.61 g/t Au, 0.17% Cu, 3.1 g/...
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Language: | English |
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University of British Columbia
2016
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Online Access: | http://hdl.handle.net/2429/57001 |