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This document summarizes a study of the Balatoc Diatreme, which hosts mineralization at the large Acupan gold deposit in the Philippines. The Balatoc Diatreme is a volcanic-hydrothermal breccia complex that provides structural control and pathways for fluid flow, resulting in epithermal mineralization. Mineralization occurred in five stages and involved boiling and fluid mixing processes. Fluid inclusion and isotope data help characterize the ore-forming fluid conditions and environments. The study emphasiz

Author

Leoniwin Keith Serrada

Language

EN