摘要
通过对泡金山锡矿床的地质特征及控矿因素的研究,分析认为地层、构造、岩浆岩对矿床的形成起了不同的控制作用,成矿受断裂构造、地层控制,具高—中温热液裂隙充填交代型和层控—矽卡岩型锡矿床特征。
Based on the study of geological features and control factors of Paojinshan Tin deposit,it’s found that strata, structure and magmatic rock play different roles in controlling the formation of ore deposits, and mineralization is controlled by the structure of fracture and strata, and it is featured by highmedium temperature hydrothermal fracture filling replacement type and stratabound-skarn Tin deposit.
作者
毕艳玲
吴南川
宾文梁
胡玉灵
Bi Yanling;Wu Nanchuan;Bin Wenliang;Hu Yuling(The First Team of Hunan Nonferrous Geological Prospecting Bureau, Chenzhou Hunan 423000;Southern Hunan Institute of Geology and Survey, Chenzhou Hunan 423000)
出处
《国土资源导刊》
2016年第4期14-19,共6页
Land & Resources Herald
关键词
锡矿床
地质特征
成因分析
泡金山
湖南
Tin deposit
geological features
genetic analysis
Paojinshan
Hunan
