Hai Jiang

Peking University

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Shao‐Yong Jiang

China University of Geosciences

Kui-Dong Zhao

China University of Geosciences

Wenqian Li

Chinese Academy of Sciences

Shui‐Yuan Yang

China University of Geosciences

Shang Shao

Yong In University

Ning-Jun Peng

China University of Geosciences

Di Zhang

China University of Geosciences

Huichuan Liu

China University of Petroleum, Beijing

Kebo Wei

Chengdu University of Traditional Chinese Medicine

Ying Liu

Hebei Normal University

Cooperative Institutions

China University of Geosciences

Chinese Academy of Sciences

Nanjing University

China University of Geosciences (Beijing)

Chengdu University of Traditional Chinese Medicine

Guangzhou Institute of Geochemistry

University of Chinese Academy of Sciences

Xiamen University

Ministry of Natural Resources

Sun Yat-sen University

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Genesis of the Zhijiadi Ag-Pb-Zn Deposit, Central North China Craton: Constraints from Fluid Inclusions and Stable Isotope Data

Geofluids (2017)

Tao Liu Suo‐Fei Xiong Shao‐Yong Jiang Hualiang Li Qi-Zhi Chen

The Zhijiadi Ag-Pb-Zn deposit is located in the central North China Craton. Fluid inclusions (FIs) studies indicate three types of FIs, including aqueous, aqueous-carbonic, and daughter mineral-bearing multiphase inclusions. The daughter minerals in FIs are mainly composed of marcasite, chalcopyrite, calcite, and dolomite. Microthermometric data show that the homogenization temperature and salinity of FIs decrease gradually from early to late stages. Homogenization temperatures from early to main to late stages span from 244 to 334°C, from 164 to 298°C, and from 111 to 174°C, respectively, while their salinities are 4.0–9.9 wt.% NaCl equiv., 0.5–12.7 wt.% NaCl equiv., and 0.2–8.8 wt.% NaCl equiv., respectively. Trapping pressures drop from 203–299 MPa (the early stage) to 32–158 MPa (the main stage). The dropping of pressure and temperature and mixing and/or dilution of ore-forming fluids result in the formation of ore deposit. Combined with C-O-S-Pb isotopic compositions, the initial ore-forming fluids and materials were likely derived from a magmatic system. As a whole, we proposed that this deposit belongs to medium-low temperature hydrothermal deposit related to volcanic and subvolcanic magmatism strictly controlled by the fault zones.

Ore genesis

Magmatic water

10.1155/2017/4153618

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Citations (14)

Highly fractionated Jurassic I-type granites and related tungsten mineralization in the Shirenzhang deposit, northern Guangdong, South China: Evidence from cassiterite and zircon U-Pb ages, geochemistry and Sr-Nd-Pb-Hf isotopes

Lithos (2018)

Hai Jiang Shao‐Yong Jiang Wenqian Li Kui-Dong Zhao Ning-Jun Peng

Cassiterite

Wolframite

Greisen

Porphyritic