Ore-forming fluids of Xishimen skarn iron deposit, China

被引:0
|
作者
Shi Saidung
V. I. Starostin
V. Yu. Prokofiev
机构
[1] Moscow State University,Geological Faculty
[2] Russian Academy of Sciences,Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
来源
Geology of Ore Deposits | 2017年 / 59卷
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摘要
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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页码:176 / 182
页数:6
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