Investigation on mineralogy, geochemistry and fluid inclusions of the Goushti hydrothermal magnetite deposit, Fars Province, SW Iran: A comparison with IOCGs

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• 作者：Mohammad Ali Rajabzadeh ; ^{rajabzad@susc.ac.ir} ; ^{mrajabzadeh@shirazu.ac.ir} ; Soqra Rasti ^{azam.rasti@yahoo.com}
• 关键词：Magnetite ; Mineralogy ; Geochemistry ; Fluid inclusion ; Iron ; Iran
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：April 2017
• 年：2017
• 卷：82
• 期：Complete
• 页码：93-107
• 全文大小：5008 K
• 卷排序：82

文摘

The Goushti hydrothermal iron deposit is hosted by the Early Mesozoic silicified dolomite. Magnetite is the major ore mineral that mainly occurs as open space fillings. A decrease in T and P supplemented by fluid mixing controls the iron oxide precipitation. The Goushti iron ore deposit could not be classified as a member of the IOCGs.