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四川省攀枝花钒钛磁铁矿床位于攀枝花境内,是我国最大的钒钛磁铁矿床。攀枝花钒钛磁铁矿矿床大地构造位置处于康滇地轴中段,区内各时代地层出露较为齐全,地质构造较为复杂,新构造运动强烈,主要形成一系列以北西-北西西向、南北向为主的断裂,区内岩浆岩十分发育,以二叠纪峨眉山玄武岩和基性-超基性岩为主。本文基于最新勘察研究成果,以岩石学、矿物学和地球化学为依据,来探讨四川省攀枝花
The Panzhihua vanadium-titanium magnetite deposit in Panzhihua is the largest vanadium-titanium magnetite deposit in China. The geotectonic location of the Panzhihua vanadium-titanium magnetite deposit is located in the middle section of the Kang-Dian axis. The stratigraphic exposures of the various periods in the area are quite complete, the geological structure is more complex, and the Neotectonic movement is intense. A series of mainly northwest-northwest-west and north-south directions are mainly formed The magmatic rocks in the area are well developed and are mainly dominated by Permian Emeishan basalts and basic-ultrabasic rocks. Based on the latest investigation and research results, based on petrology, mineralogy and geochemistry,