广西金秀龙围铜矿矿床成因  

THE GENESIS OF LONGWEI CU DEPOSIT IN JINXIU,GUANGXI

作　　者：吴荣华[1] 庞保成[1,2] 黄淑娟 张敏 李泽江[1] 

机构地区：[1]桂林理工大学地球科学学院,广西桂林541004 [2]广西地质工程中心重点实验室,广西桂林541004 [3]南宁市曙光矿业有限公司,广西南宁530022

出　　处：《云南地质》2012年第1期121-124,127,共5页Yunnan Geology

摘　　要：矿体赋存于下泥盆系莲花山组上段紫红色砂岩的断裂破碎带中,受近南北断层破碎带控制明显,成矿物质来源与构造运动作用引发的地下深部流体密切相关。矿床属中低温热液硫化物充填—交代型。The ore body exists in the fault fracture zone of Lower Devonian LianhuashanFormation Upper Member purple sandstone,which is controlled clear by nearly SN fault fracture zone.The source of metallogenetic material is close related with the deep fluid caused by the structural activity.The ore deposit belongs to the type of middle-low T hydrothermal sulfide filling-metasomatism.

关 键 词：脉状铜矿 断层破碎带 充填—交代 包裹体 广西金秀龙围 

分 类 号：P618[天文地球—矿床学]