贵州省排庭金矿地质特征与成因分析  

Geological characteristics of the Paiting Au deposit with its genesis analysis,Guizhou Province

作　　者：伍守荣[1] 

机构地区：[1]昆明理工大学国土资源工程学院

出　　处：《矿产与地质》2008年第1期55-61,共7页Mineral Resources and Geology

基　　金：国家资源补偿费矿产资源勘查项目(项目编号:200601003)

摘　　要：排庭金矿是贵州三都——丹寨锑、汞、金成矿带上,继苗龙锑-金矿、宏发厂汞-金矿后首次发现的产于中下寒武统独立型的微细浸染型金矿,其矿体受断裂构造、地层、岩性等因素控制,矿床规模为中型。对该矿床的地质特征及成因进行总结和分析,对于华南褶皱带与扬子准地台过渡带寻找寒武纪地层中的微细浸染型金矿具有重要的借鉴和指导意义。The Paiting Au deposit is a Mid-Lower Cambrian independent micrograined disseminated gold mine occurred in Sandu-Danzhai metallogenic belt for Sb,Hg, Au deposits, which has been firstly found afer the discovery of Miaolong Sb-Au deposit, Hongfachang Hg-Au deposit. The orebodies of the Pairing Au deposit, which is a middle scale depsoit, are controlled by the factors of fault structure,strata and lithology etc. It has concluded and analyzed the geological characteristics and the genesis of this deposit, which will be a significant reference and guidance for the prospecting of Cambrian micrograined disseminated Au deposit in the transition zone between South China fold belt and Yangtze paraplatform.

关 键 词：金矿 成因分析 地质特征 排庭 贵州 

分 类 号：P618.51[天文地球—矿床学]