我国主要成矿地质作用及常见矿床类型  

Main metallogenetic geological processes and conventional deposit types in China

作　　者：王玉往[1,2] 叶天竺[3] 王京彬[1,2] 吕志成[3] 韦昌山[3] 廖震[2] 张会琼[2] 

机构地区：[1]中色地科矿产勘查股份有限公司,北京100012 [2]北京矿产地质研究院,北京100012 [3]中国地质调查局发展研究中心,北京100083

出　　处：《矿产勘查》2014年第2期111-123,共13页Mineral Exploration

基　　金：中国地质调查局危机矿山项目(编号:200699105);老矿山项目(编号:121200113086300)共同资助

摘　　要：文章主要从找矿预测角度较系统梳理了我国常见的(金属)矿床类型,讨论了矿床类型与成矿地质作用和成矿地质体的关系。将我国主要成矿地质作用分为沉积地质作用、火山地质作用、侵入岩浆地质作用、变质地质作用、大型变形地质作用以及复合/叠加地质作用6类,并进一步划分出16个成矿地质作用亚类,共32种常见矿床类型。对每一类成矿地质作用和矿床类型的含义和特点进行了解释和说明。From the prospecting prediction viewpoint, this paper systematically sorts out the conventional ore deposit types in China and discusses the relationship among the deposit type, metallogenetic geological processes and ore - forming geological body. The main metallogenetie geological processes in China can be classified into six types such as sedimentary, volcanic, intrusive magmatic, metamorphic, large deformation and superposed/superimposed metallogensis typies. Furthermore, sixteen subtypes of geological processes of metallogensis and thirty two conventional ore deposit types are also identified. Connotation and characteristics of each geo- logical process type and deposit type are descripted and illustrated in the paper.

关 键 词：成矿地质作用 成矿地质体 矿床类型 典型矿床 

分 类 号：P618[天文地球—矿床学]