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攀枝花钒钛磁铁矿床处于扬子地台西缘,康滇地轴中南段,是峨眉山大火成岩省的重要组成部分。前人研究认为钛磁铁矿在空间上和成因上均与含矿母岩有着密切关系,其成矿过程与成岩过程紧密相关(刘英俊,1979)。攀枝花含矿母岩的岩石类型主要有浅色-深色磁铁矿辉长岩和块状钛铁氧化物矿石,本次研究通过野外观察,显微镜下鉴定以及扫描电镜对主要含矿岩体进行了分析测试,对作为重要金属氧化物之一的钛铁矿在组构和成分上有了进一步的认识。
The Panzhihua vanadium-titanium magnetite deposit is located at the western margin of the Yangtze Platform and the central-southern part of the Kangdi-Dian axis. It is an important part of the Emeishan large igneous province. Previous studies suggest that the titanomagnetite is closely related to ore-bearing parent rocks both in space and genesis, and its mineralization is closely related to diagenesis (Liu, 1996). The rock types of the Panzhihua ore-bearing parent rocks are mainly light-dark magnetite gabbro and massive titanium iron oxide ores. Through the field observation, microscopic identification and scanning electron microscopy, the main ore-bearing rock masses Analytical testing has given further insight into the structure and composition of ilmenite, one of the most important metal oxides.