Email this article Ore-forming fluids of Xishimen skarn iron deposit, China
- Authors: Saidung S.1, Starostin V.I.1, Prokofiev V.Y.2
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Affiliations:
- Geological Faculty
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Issue: Vol 59, No 2 (2017)
- Pages: 176-182
- Section: Article
- URL: https://ogarev-online.ru/1075-7015/article/view/215165
- DOI: https://doi.org/10.1134/S1075701517020027
- ID: 215165
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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.
About the authors
Shi Saidung
Geological Faculty
Email: vpr2004@rambler.ru
Russian Federation, Moscow, 119991
V. I. Starostin
Geological Faculty
Email: vpr2004@rambler.ru
Russian Federation, Moscow, 119991
V. Yu. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Author for correspondence.
Email: vpr2004@rambler.ru
Russian Federation, Moscow, 119017
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