摘要
乱安子铁铅锌多金属矿位于秦岭造山带西段腹地的中秦岭南缘华西力-印支期褶皱带与南秦岭北缘印支褶皱带的衔接部位。先后发现了大中型的铁铅锌多金属矿多处,为此文章主要对矿体地质特征及找矿潜力进行分析,为寻找多金属矿提供理论依据。
Luanzi Fe Pb Zn polymetallic deposit is located at the junction of the huaxili Indosinian fold belt in the southern margin of middle Qinling and the Indosinian fold belt in the northern margin of South Qinling.Many large and mediumsized iron lead-zinc polymetallic deposits have been found.Therefore,this paper mainly analyzes the geological characteristics and prospecting potential of the ore body,so as to provide a theoretical basis for looking for polymetallic deposits.
作者
宋全红
SONG Quan-hong(Tianshui Mineral Exploration Institute of Gansu Nonferrous Metal Geological Exploration Bureau,Tianshui 741020,China)
出处
《世界有色金属》
2021年第5期87-88,共2页
World Nonferrous Metals
关键词
多金属矿
地质特征
找矿潜力
polymetallic deposit
geological characteristics
prospecting potential
