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Constraints of fluid inclusions and in-situ S-Pb isotopic compositions on the origin of the North Kostobe sediment-hosted gold deposit, eastern Kazakhstan
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文摘
Paleozoic orogenic gold deposits in eastern Kazakhstan Ore fluids were mesothermal, CO2-rich and low salinity. Fluids were generated from sedimentary rocks by metamorphic devolatilization. In-situ measurement of S and Pb isotopes on sulfides by LA-MC-ICPMS

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