攀枝花钒钛磁铁矿成矿地质特征与成矿规律初探  

Panzhihua vanadium titanium magnetite mineralization geological characteristics and metallogenic regularity

作　　者：李玥[1,2] 刘严松[1,2] 刘建伟[1,2] 王梦潇[1,2] 郝江波[1,2] 

机构地区：[1]国土资源部构造成矿成藏重点实验室(成都理工大学),成都610059 [2]成都理工大学地球科学学院,成都610059

出　　处：《世界有色金属》2017年第1期95-95,97,共2页World Nonferrous Metals

基　　金：中地调局"攀枝花深部找矿疑难问题研究(1212011220867)";成都理工大学"江浪矿田构造与成矿研究"联合资助

摘　　要：攀枝花钒钛磁铁矿位于攀西大裂谷构造岩浆岩带,根据其所处地质环境大致推测攀枝花钒钛磁铁矿的形成机理是由于地幔物质上涌形成岩浆,本文基于对矿区进行野外地质调查,结合前人研究基础上对其成矿地质特征与成矿规律进行阐述。Panzhihua vanadium-titanium magnetite is located in the Panxi large rift tectonic magmatic rock belt. According to its geological environment, it is presumed that the formation mechanism of Panzhihua vanadimn-titanomagnetite is due to the upwelling of mantle material. Based on the field geology Based On the previous studies, the metallogenic characteristics and metallogenic regularities of the ore deposits are expounded.

关 键 词：钒钛磁铁矿 成矿规律 成矿地质特征 

分 类 号：P618.31[天文地球—矿床学]