云南兰坪县核桃箐铜矿成矿条件及矿床成因  

THE METALLOGENESIS CONDITION AND GENESIS OF HETAOQING CU DEPOSIT IN LANPING,YUNNAN

作　　者：林焱一 李良旭[1] 张辉尧[1] 

机构地区：[1]国土资源部昆明矿产资源监督检测中心,云南昆明650218

出　　处：《云南地质》2017年第1期30-33,共4页Yunnan Geology

摘　　要：兰坪核桃箐铜矿矿体与区内的次级断裂构造活动有着密切的关系,矿体的分布、规模、形态和产状都严格受断层破碎带的控制,该铜矿属中低温热卤水铜矿床。The ore body of Hetaoqing Cu Deposit in Lanping is in close relation with the secondary fault in this area. The distribution,scale,form and occurrence of ore body are controlled strictly by the fault fracture zone. It belongs to the middle-low T hot brine Cu deposit.

关 键 词：断裂构造控矿 中低温热卤水铜矿床 云南兰坪核桃箐. 

分 类 号：P618.41[天文地球—矿床学]