Geology, alteration and mineralization on the Hank property, northwestern British Columbia : a near-surface, low-sulfidation epithermal system
Hydrothermal alteration on the Hank property, northwestern British Columbia, is hosted by andesitic to basaltic volcaniclastic breccias, flows and sills of the Upper Triassic Stuhini Group; Lower Jurassic sedimentary rocks; and, a hypabyssal, Middle Jurassic (185±3 Ma) potassiumfeldspar megacryst...
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| Format: | Others |
| Language: | English |
| Published: |
2009
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| Online Access: | http://hdl.handle.net/2429/5768 |