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The document discusses epithermal mineralization in the Bonanza-Sandy vein system in the Masara Gold District of Mindanao, Philippines. It describes three stages of mineralization, with the first stage being the main gold mineralization phase. The deposit exhibits characteristics of intermediate sulfidation epithermal deposits based on mineral assemblages and alteration minerals. Hydrothermal fluids from a nearby intrusive complex likely formed the first stage veins, with later stages involving boiling flui

Author

ajreateguic

Language

EN