Ore-forming fluids of Xishimen skarn iron deposit, China

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 hi...

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Veröffentlicht in:	Geology of ore deposits 2017-03, Vol.59 (2), p.176-182
Hauptverfasser:	Saidung, Shi, Starostin, V. I., Prokofiev, V. Yu
Format:	Artikel
Sprache:	eng
Schlagworte:	Calcite Calcium magnesium silicates Computational fluid dynamics Diopside Earth and Environmental Science Earth Sciences Fluid inclusions Fluids Iron Mineral Resources Minerals Ores Sodium chloride Solutions Temperature
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Beschreibung
Zusammenfassung:	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.
ISSN:	1075-7015 1555-6476
DOI:	10.1134/S1075701517020027