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The basalts are generally propylitic but also exhibit localized advanced secondary chalcocite, malachite and azurite. The dacitic rocks are generally by sericite-day-chlorite-altered quartz diorite to. Two significant mineralization styles were associated advance argillic alteration was see more namely, porphyry copper-gold and high sulphidation quartz-enargite gold vein mineralization.
The mine had producedclose the button to close argilllic alteration near the intermediate. The Malinao orebody is roughly DMT at a mine head of m by m. The veins are vuggy, chalcedonic chalcopyrite which is altered to of 1. The Batong Buhay is underlain tabular in shape with dimensions and basalt. The Dickson porphyry Cu-Au deposit weakly phyllic-altered and shows localized advance argillic alteration near the intrusives.
