Ore-Forming Fluids of Xishimen Skarn Iron Deposit, Chinaстатья
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Дата последнего поиска статьи во внешних источниках: 24 июня 2017 г.
Аннотация: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.