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The Sharang porphyry Mo deposit is the first discovered Mo porphyry‐type deposit in the Gangdese Metallogenic Belt. The orebody is hosted by the Eocene multi‐stage composite intrusive complex which is emplaced in the Upper Permian Mengla Formation and cut by the Miocene dykes. Granite porphyry is recognized as the ore‐bearing porphyry in the complex, which consists of quartz diorite, quartz monzonite,...
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