摘要
内蒙古达斯呼都格矿区位于得尔布干成矿带西南段。其大地构造位置为兴安地槽褶皱系之Ⅱ级构造单元额尔古纳兴凯地槽褶皱带。区域内矿床类型以斑岩型及火山、次火山热液型矿床最多,占工业储量的绝大多数,通过对内蒙古达斯呼都格已有勘查成果与区域已知矿床成矿特征综合对比分析后认为本区具有寻找斑岩型铜矿的潜力。
Dahuduge mining area in Inner Mongolia is located in the southwest of Derbugan metallogenic belt.Its geotectonic location is Erguna Xingkai geosyncline fold belt,a class II structural unit of Xing'an geosyncline fold system.Porphyry,volcanic and subvolcanic hydrothermal deposits are the most types of deposits in the region,accounting for the vast majority of industrial reserves.Through the comprehensive comparison and analysis of the existing exploration results and the metallogenic characteristics of regional known deposits in dashuduge,Inner Mongolia,it is considered that this area has the potential to search for porphyry type copper deposits.
作者
韩效斌
支元栋
李沛龙
郎学聪
HAN Xiao-bin;ZHI Yuan-dong;LI Pei-long;LANG Xue-cong(The Third Geological Exploration Institute of China Metallgical Geology Bureau,Taiyuan 030000,China)
出处
《世界有色金属》
2022年第9期172-174,共3页
World Nonferrous Metals
关键词
内蒙古
达斯呼都格
斑岩型铜矿
Inner Mongolia
Darth hudug
porphyry copper deposit
