Magnetite as an indicator mineral in till: a test using the Mount Polley porphyry Cu-Au deposit, British Columbia
In the Canadian Cordillera, Mesozoic calcalkaline and alkaline intrusive igneous rocks that are prospective for hosting porphyry Cu-Au mineralization may be overlain by thick glacial overburden. Previous studies have shown that magnetite from ore deposits has a unique trace element signature that di...
| Main Author: | |
|---|---|
| Other Authors: | |
| Language: | English en |
| Published: |
2015
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1828/6992 |