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New phase relations in the Cu–Fe–S system at 800°C; constraint of fractional crystallization of a sulfide liquid

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Gold solubility, speciation, and partitioning as a function of HCl in the brine-silicate melt-metallic gold system at 800 o C and 100 MPa

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CO₂-rich fluid inclusions with chalcopyrite daughter mineral from the Fenghuangshan Cu–Fe–Au deposit, China: implications for metal transport in vapor

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