云南省东川汤丹铜矿床地质特征与矿床成因浅析  

Geological Features and Genesis of the Tang Dan Copper Deposit in Dongchuan of Yunnan Province

作　　者：尹琼[1] 

机构地区：[1]昆明冶金高等专科学校矿业学院,云南昆明650033

出　　处：《昆明冶金高等专科学校学报》2016年第5期17-21,27,共6页Journal of Kunming Metallurgy College

摘　　要：在分析云南省东川铜矿区区域成矿地质背景的基础上,对其范围内的汤丹铜矿床矿区地质及矿体地质特征进行了深入剖析,总结其矿床成因,认为该矿床成因属于沉积—变质—改造综合作用而形成。Based on the analysis of the metallogenic geological background of the Dongchuan copper deposit in Yunnan Province,geology and orebody geological characteristics of Tangdan copper deposit in the area are analyzed. The genesis of the deposit is summarized,and it is believed that the genesis of this deposit belongs to the combination of sedimentary- metamorphism- reforming.

关 键 词：汤丹铜矿床 地质特征 矿床成因 

分 类 号：TD163.2[矿业工程—矿山地质测量]