摘要
西铅炉子铅锌矿主要是受到断裂和石英脉联合控制,主要断裂为北西(北北西)向断裂为主。岩浆活动发生多次变形变质,成矿地质特征明显,取得了较好的地质成果,对以后发展指明方向。
The lead-zinc deposit in Xilianluozzi is mainly controlled by faults and quartz veins,and the main faults are NW (NW) trending faults.The magmatic activity has undergone multiple deformations and metamorphisms,and the metallogenic geological features are obvious,and good geological results have been achieved,pointing out the direction for future development.
作者
胡富荣
HU Fu-rong(Lanzhou Mineral Exploration Institute of Gansu Nonferrous Metal Geological Exploration Bureau,Lanzhou 730046,China)
出处
《世界有色金属》
2022年第13期85-87,共3页
World Nonferrous Metals
关键词
西铅炉子
铅锌矿床
地质特征
找矿标志
West Lead Furnace
lead-zinc deposit
geological features
prospecting signs
