摘要
石青硐铜多金属矿床大地构造位于北祁连构造带东段,是白银地区中部酸性火山杂岩系块状硫化物铜多金属成矿带组成部分之一。通过研究本区大地构造背景、成矿地质特征等的研究,初步分析了石青硐铜多金属矿床地质特征,评价了找矿前景。
Shiqingdong polymetallic deposit tectonic structure, is located in the eastern section of the North Qilian structure, is one of component of acidic volcanic complex rock system massive sulfide in the copper polymetallic belt. This paper primarily analyzes the geological characteristics of Shiqingdong polymetallic deposit, and evaluates ore-searching prospect through studying the backgronnd of tectonic structure and geological characteristics of the ore deposit.
作者
宋小强
吴东
SONG Xiao-qiang;WU Dong(Gansu Nonferrous Metal Geological Exploration Bureau Baiyin Mineral Exploration Institute,Baiyin 730900,China)
出处
《甘肃冶金》
2018年第5期54-58,共5页
Gansu Metallurgy
关键词
铜多金属矿
地质特征
找矿前景
copper polymetallic deposit
geological characteristics
ore-searching prospect
