四川省会理县某铜矿地质特征及找矿远景分析  

Geological Characteristics and Prospecting Perspective View of a Certain Copper Mine in Huili County,Sichuan Province

作　　者：余冲[1] 李良波[1] 吴小艳[1] 廖娟[1] 姜浩杰 

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《四川建材》2015年第5期240-241,244,共3页Sichuan Building Materials

摘　　要：该矿区位于扬子地台西南缘,扬子地台西南缘经历了多期多阶段构造-岩浆活动及变质变形作用,一直是地质学者关注的构造单元和重要的成矿带。本文从该矿区成矿地质条件、矿体特征、矿石特征、矿床成因等方面进行了研究,对区内找矿远景进行了探讨,提高对该区铜矿地质特征的认识,为进一步在本区及外围找矿提供理论依据,具有一定的参考价值及指导意义。The mine area is located in the South- Western margin of the Yangtze platform,the South- Western margin of the Yangtze platform has experienced multistage- multiphase tectonic- magmatic activity and the metamorphism and deformation,it has always been the tectonic unit and important metallogenic belt which is concerned by geologists. This article is studied from the ore- forming geological conditions, ore- body characteristics, ore characteristics, ore deposit origin, etc,studies the prospecting potential,raises the awareness of the geological characteristics of copper deposit in the area,in order to provide the theoretical basis for prospecting ore deposits and its exploration,which has a certain reference value and guiding significance.

关 键 词：会理县 铜矿 地质特征 找矿远景 

分 类 号：P618.41[天文地球—矿床学]