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Ore-forming fluids of Xishimen skarn iron deposit,China
Authors:Shi Saidung  V I Starostin  V Yu Prokofiev
Institution:1.Geological Faculty,Moscow State University,Moscow,Russia;2.Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry,Russian Academy of Sciences,Moscow,Russia
Abstract:Fluid inclusions in calcite and diopside from the Xishimen skarn iron deposit in China were studied. The deposit ores were formed from chloride solutions with salinity ranging from 8.4 to 59.6 wt % NaCl equiv within the temperature range of 210 to 590°C. The model of skarn ore formation involving high-temperature magmatic fluids is discussed.
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