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Porphyry copper indicator minerals (PCIM) are defined as minerals indicative of porphyry mineralization. Identifying PCIM in surficial sediments (e.g. till and stream sediments) can serve to detect the presence of buried porphyry mineralization. This project was initiated to develop and test potential PCIM using zircon, epidote and rutile recovered from till in the region of the Gibraltar porphyry Cu-Mo deposit of south central British Columbia.

Glacial dispersal of refractory minerals from the Gibraltar porphyry copper deposit, south central British Columbia, Canada