Enviar artigo por via de e-mail Ore-forming fluids of Xishimen skarn iron deposit, China
- Autores: Saidung S.1, Starostin V.I.1, Prokofiev V.Y.2
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Afiliações:
- Geological Faculty
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Edição: Volume 59, Nº 2 (2017)
- Páginas: 176-182
- Seção: Article
- URL: https://ogarev-online.ru/1075-7015/article/view/215165
- DOI: https://doi.org/10.1134/S1075701517020027
- ID: 215165
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Resumo
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.
Sobre autores
Shi Saidung
Geological Faculty
Email: vpr2004@rambler.ru
Rússia, Moscow, 119991
V. Starostin
Geological Faculty
Email: vpr2004@rambler.ru
Rússia, Moscow, 119991
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Autor responsável pela correspondência
Email: vpr2004@rambler.ru
Rússia, Moscow, 119017
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