The Fengshan porphyry-skam copper-molybdenum deposit is located in the southeastern Hubei Province, East China.Cu-Mo mineralization is hosted in the Fengshan quartz diorite porphyry stock that intruded the Triassic Daye Formation of carbonate rocks in the early Cretaceous(ca.140 Ma),as well as in the contact zone between these two,forming
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