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This document summarizes a study of heterogeneous melt and hypersaline liquid inclusions in quartz veins from shallow porphyry-type mineralization in the Cerro de Pasco district of Peru. The mineralization consists of banded quartz-magnetite-chalcopyrite veins crosscutting trachyte porphyry and records a multiphase formation history with early high-temperature (>600°C) stages characterized by melt and hypersaline liquid inclusions, followed by a lower-temperature (<350°C) stage of sulfide precipitation. Ana

Author

Tpoma

Language

EN