电邮这篇文章 Ore-forming fluids of Xishimen skarn iron deposit, China
- 作者: Saidung S.1, Starostin V.I.1, Prokofiev V.Y.2
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隶属关系:
- Geological Faculty
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 59, 编号 2 (2017)
- 页面: 176-182
- 栏目: Article
- URL: https://journals.rcsi.science/1075-7015/article/view/215165
- DOI: https://doi.org/10.1134/S1075701517020027
- ID: 215165
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详细
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.
作者简介
Shi Saidung
Geological Faculty
Email: vpr2004@rambler.ru
俄罗斯联邦, Moscow, 119991
V. Starostin
Geological Faculty
Email: vpr2004@rambler.ru
俄罗斯联邦, Moscow, 119991
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
编辑信件的主要联系方式.
Email: vpr2004@rambler.ru
俄罗斯联邦, Moscow, 119017
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