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The Huangshan gold deposit is hosted in the ductile shear zone of the metamorphosed Precambrian Chencai Group in the Jiangshan-Shaoxing fault zone between the Yangtze and the Cathaysia blocks. The mineralization can be divided into three stages: pre-ore stage barren quartz-sericite veins, ore stage quartz-pyrite veins, and post-ore stage calcite-quartz veins. A combination of fluid inclusion microthermometry...
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