The southwest zone breccia-centered silica-undersaturated alkalic porphyry Cu-Au deposit, Galore Creek, B.C : magmatic-hydrothermal evolution and zonation, and a hydrothermal biotite perspective
Situated in northwest B.C Canada, the Southwest Zone Cu-Au breccia-centered deposit is one of twelve mineralized centers in the Galore Creek alkalic porphyry district. Formed in an island arc-setting outboard of ancestral North America in the lateTriassic, deposits in the Galore Creek district have...
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| Format: | Others |
| Language: | English |
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University of British Columbia
2009
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| Online Access: | http://hdl.handle.net/2429/15005 |