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The Laoshankou Fe-Cu-Au deposit is located at the northern margin of Junggar Terrane, Xinjiang, China. This deposit is hosted in Middle Devonian andesitic volcanic breccias, basalts, and conglomerate-bearing basaltic volcanic breccias of the Beitashan Formation. Veined and lenticular Fe-Cu-Au orebodies are spatially and temporally related to diorite porphyries in the ore district. Wall-rock alteration...
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