In most porphyry copper deposits, acoustic copper minerals chalcopyrite (CuFeS 2). However, secondary copper sulfide is often formed due to strong alteration and oxidation, such as chalcopyrite (Cu 2 S), copper ore (Cu 4 FeS), and copper blue (CuS). In the oxidation zone of the copper- molybdenum deposit, the iron content is unchanged. However, when groundwater transports copper ions, copper ions react rapidly with chalcopyrite and pyrite to form secondary copper minerals.

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