云南维西县巴丁吉格铜矿成矿规律  

THE METALLOGENESIS RULE OF BADINGJIGE CU DEPOSIT IN WEIXI,YUNNAN

作　　者：张云龙[1] 李昊[1] 李维忠[1] 

机构地区：[1]云南省地质矿产勘查院,云南昆明650051

出　　处：《云南地质》2016年第2期157-161,共5页Yunnan Geology

摘　　要：巴丁吉格铜矿矿体呈层状、脉状主要沿矿区中一组次级断裂带分布,同时矿体的就位,又受地层中侏罗统花开左组中不同岩性转换界面—砂质泥岩与灰岩转换界面的控制,为热液砂岩型铜矿。The ore body of Badingjige Cu deposit is bedded, veined, distributed mainly along a secondary fault zone. And the emplacement of ore body is controlled by the transformation interface of different lithological character in Middle Jurassic Huakaizuo Formation, transformation interface of sandy mudstone and limestone. It is a hydrothermal sandstone Cu deposit.

关 键 词：砂岩型铜矿 构造地层控矿 云南维西巴丁吉格 

分 类 号：P618.41[天文地球—矿床学]