摘要
在对该区进行岩浆岩、地球化学、矿床物质组分特征研究的基础上 ,根据所处构造区带、岩浆岩及成矿特征 ,划分出三个矿床成矿系列 ,即 :东部后加里东隆起区与燕山期中浅成酸性花岗岩有关的钨锡银矿床成矿系列、西部海西 -印支坳陷区燕山期中浅成酸性中酸性花岗岩有关的铜钼铅锌银 (金 )矿床成矿系列和中部过渡带钨锡铋钼 (铅锌银 )矿床成矿系列。
Based on research of the magmatic rocks, geochemistry and metallogenetic materials of ore deposits , three deposit metallogenetic series have been divided across the Chenzhou Linwu deep seated fault, ie., the W Sn Ag series related to the Yanshanian hypabassal acid granites in the post Caledonian uplift area at the east part, the Cu Mo Pb Sn Ag (Au) series related to Yanshanian hypabassal middle acid granites in the depression area of Hercynian Indosinian Epoch at the west part and the W Sn Bi Mo(Pb, Zn,Ag) series at central transitional belt.
出处
《华南地质与矿产》
CAS
2000年第3期34-41,共8页
Geology and Mineral Resources of South China
基金
地质矿产部"八五"科技攻关项目"武夷-云开典型成矿区矿产预测"二级课题"罗霄-武夷隆起区成矿地质环境和成矿预测研究"下属三级专题"湖南郴州-临武断裂带两侧成矿预测及靶区优选"(85-01-007-01-1)的部分成果
关键词
钨锡铅锌金银矿床
成矿系列
郴州-临武断裂带
湖南
=
W-Sn-Pb-Zn-Au-Ag deposits
deposit metallogenetic series
Chenzhou-Linwu fault belt
Hunan
