川西南拉一木玄武岩型铜矿地质特征及成因探讨  

Geological characteristics and genesis of the laimu basaltic copper deposit in southwest sichuan province

作　　者：赵勇 胥明 ZHAO Yong;XU Ming(280 Institute of Nuclear Industry,Guanghan 618300,China)

机构地区：[1]核工业二八0研究所,四川广汉618300

出　　处：《世界有色金属》2018年第24期76-77,共2页World Nonferrous Metals

摘　　要：对川西南拉一木地区的峨眉山玄武岩分布,岩性特征;介绍了矿化蚀变带的规模,矿化蚀变情况等;初步探讨了成因类型;并从岩性、构造、蚀变等找矿标志进行了初步分析和总结,为下一步的找矿提供依据。The distribution and lithological characteristics of Emeishan basalt in Layimu area, southwestern Sichuan Province, the scale of mineralized alteration zone and the situation of mineralized alteration are introduced, the genetic types are preliminarily discussed, and the prospecting indicators such as lithology, structure and alteration are preliminarily analyzed and summarized to provide basis for further prospecting.

关 键 词：玄武岩 铜矿 地质特征 拉一木 

分 类 号：P618.41[天文地球—矿床学]