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Deposit | Fluid inclusion type | Homogenization temperature | Salinity | Initial ore-forming fluids | Metallogenic epoch | Analytical methods | Geodynamic setting | Reference |
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Chehugou | CO2-bearing multiphase daughter mineral-bearing multiphase liquid-rich two-phase gas-rich two-phase pure gas phase | Early: 400–270°C Middle: 370–160°C Late: 230–120°C | Early: 58.41–1.06% Nacleqv Middle: 48.21–0.88% Nacleqv Late: 8.41–0.71% Nacleqv | High temperature, high salinity, CO2-bearing, CO2-NaCl-H2O system | 250.2 ± 7.2 Ma | Molybdenite Re-Os dating | Postcollision local extension | [1, 2] |
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Jiguanshan | CO2-bearing multiphase daughter mineral-bearing multiphase liquid-rich two-phase gas-rich two-phase pure CO2-bearing pure liquid phase | Early: >480°C Middle: 480–320°C Late: 320–180°C | Early: >66.75% Nacleqv Middle: 56.76–4.65% Nacleqv Late: <10.86% Nacleqv | High temperature, high salinity, CO2-bearing, high oxygen fugacity, magmatic hydrothermal | 151.1 ± 1.3 Ma | Molybdenite Re-Os dating | Tectonic regime transformation | [3, 4] |
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Aolunhua | CO2-bearing multiphase daughter mineral-bearing multiphase liquid-rich two-phase gas-rich two-phase pure gas phase | Early: 430–330°C Middle: 350–250°C Late: 270°C | Early: 58.41–1.06% Nacleqv Middle: 48.21–0.88% Nacleqv Late: 8.41–0.71% Nacleqv | High temperature, high salinity, CO2-bearing, high oxygen fugacity, CO2-NaCl-H2O system | 129.4 ± 3.4 Ma | Molybdenite Re-Os dating | Continental extension related to lithosphere thinning | [13], Ma et al., 2009 |
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Daheishan | CO2-bearing multiphase daughter mineral-bearing multiphase gas-liquid two-phase | Early: 391–286°C Late: 379–232°C | Early: 44–3% Nacleq Late: 9–1% Nacleqv | Medium-high temperature, high salinity, NaCl-H2O system | 168.2 ± 3.2 Ma | Molybdenite Re-Os dating | Active continental margin or island arc | [6, 7, 14] |
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Luming | Daughter mineral-bearing multiphase liquid-rich two-phase gas-rich two-phase CH4-bearing | 449–133°C | 53.1–1.2% Nacleqv | High temperature, medium salinity NaCl-H2O±CH4 system | 176.7 ± 4.4 Ma | Molybdenite Re-Os dating | Plate subduction | [23] |
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Fu’anpu | Gas-liquid two-phase | 257.8–123.8°C | 17.47–1.39% Nacleqv | Medium-low temperature, medium salinity NaCl-H2O ± CH4 system | 168.22 ± 0.87 Ma | Molybdenite Re-Os dating | Plate subduction | [11] |
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