Late Eocene tectono-magmatic evolution and genesis of reduced porphyry copper-gold mineralization at the North Fork deposit, west central Cascade Range, Washington, U.S.A.
The North Fork porphyry Cu-Au deposit is located in the west central Cascades Mountain Range, Washington, U.S.A., and belongs to a belt of Eocene to Miocene porphyry Cu (Au) deposits that extend northward into the Coast Mountains of southern British Columbia. The deposit has a geological reserve...
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| Format: | Others |
| Language: | English |
| Published: |
2009
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| Online Access: | http://hdl.handle.net/2429/15188 |