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The geology and geochronology of the Waifangshan Mo-quartz vein cluster in eastern Qinling, China
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文摘
Molybdenites from the Waifangshan area yield a mean Re–Os age of ~ 242 Ma. Waifangshan Mo-quartz vein cluster form an orogenic type Mo system in Qinling. Re contents of the molybdenite suggest the fluids were sourced from old crust. Continental arc to back-arc transitional area accommodates Waifangshan Mo deposit.

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