Characteristics of the hydrothermal system of the porphyry copper (gold) deposit at Shaxi, Eastern China
Qijang Ren, Bing Fu, Wenxuan Hu, Wenyi Xu, Zhenhao Duan, Nancy Møller, John H. Weare
Abstract
Qijang Ren, Bing Fu, Wenxuan Hu, Wenyi Xu, Zhenhao Duan, Nancy Møller, John H. Weare
Abstract
The porphyry copper (gold) deposit at Shaxi is a special and large size deposit in eastern China. In the ore-forming process, the water and ore-forming materials in ore solution were magmatic in origin. Systematic studies of fluid inclusions reveal that the ore-forming system was characterized by relatively high temperature and low pressure as well as high contents of CO 2 and NaCl. Great amounts of evidence support that the fluid immiscibility played an important part in the formation of Shaxi porphyry copper (gold) deposits.
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The porphyry copper (gold) deposit at Shaxi is a special and large size deposit in eastern China. In the ore-forming process, the water and ore-forming materials in ore solution were magmatic in origin. Systematic studies of fluid inclusions reveal that the ore-forming system was characterized by relatively high temperature and low pressure as well as high contents of CO 2 and NaCl. Great amounts of evidence support that the fluid immiscibility played an important part in the formation of Shaxi porphyry copper (gold) deposits.
Key concepts: China, Hydrothermal circulation, Porphyry copper deposit, Geochemistry, Geology, Copper, Metallurgy, Geography