The geology and geochronology of the Waifangshan Mo-quartz vein cluster in eastern Qinling, China
Abstract
The Waifangshan Mo-quartz vein cluster occurs at the northernmost margin of the Qinling Orogen. The orebodies occur as quartz veins and are controlled by low-angle faults. We identify three hydrothermal stages, characterized by veinlets of quartz–pyrite, quartz–molybdenite–pyrite–chalcopyrite–galena–sphalerite, and quartz–carbonate assemblages, respectively. The early-stage quartz veins were structurally-deformed, brecciated, and filled by...
Paper Details
Title
The geology and geochronology of the Waifangshan Mo-quartz vein cluster in eastern Qinling, China
Published Date
Mar 1, 2017
Journal
Volume
81
Pages
548 - 564
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