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