Мақаланы E-mail арқылы жіберу Ore-forming fluids of Xishimen skarn iron deposit, China
- Авторлар: Saidung S.1, Starostin V.I.1, Prokofiev V.Y.2
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Мекемелер:
- Geological Faculty
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Шығарылым: Том 59, № 2 (2017)
- Беттер: 176-182
- Бөлім: Article
- URL: https://journals.rcsi.science/1075-7015/article/view/215165
- DOI: https://doi.org/10.1134/S1075701517020027
- ID: 215165
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Аннотация
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.
Авторлар туралы
Shi Saidung
Geological Faculty
Email: vpr2004@rambler.ru
Ресей, Moscow, 119991
V. Starostin
Geological Faculty
Email: vpr2004@rambler.ru
Ресей, Moscow, 119991
V. Prokofiev
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Хат алмасуға жауапты Автор.
Email: vpr2004@rambler.ru
Ресей, Moscow, 119017
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