Research on Superimposed Metallogenic System  

作　　者：ZhaiYusheng WangJianping DengJun PengRunmin 

机构地区：[1]KeyLaboratoryofLithosphericTectonicsandLithoprobingTechnology,ChinaUniversityofGeosciences,MinistryofEducation,Beijing100083,China

出　　处：《Journal of China University of Geosciences》2004年第1期9-14,共6页中国地质大学学报（英文版）

基　　金：ThepaperisfinanciallysupportedbytheKeyProgramoftheNationalNaturalScienceFoundationofChina (No .40 2 340 51 )andtheStateKeyBasicResearchandDevelopmentPlanofChina (No.2 0 0 1CB40 980 7)

摘　　要：As located in the junction of three tectonic plates (the Eurasian plate, the Indian plate and the west Pacific plate), the China continent shows complex regional metallogenic features due to tectonic evolution of “micro-plates, polycycle tectonic movements”. Well developed superimposed metallogenic systems have constituted one of the regional metallogenic features in China. Through the study on superimposed metallogenic system of the middle and lower reaches of the Yangtze River and of the Yuebei basin (northern Guangdong Province), the authors put forward some basic combination pattern of sedimentary-magmatic superimposed metallogenic system and summarize its forming conditions (controlling factors).As located in the junction of three tectonic plates (the Eurasian plate, the Indian plate and the west Pacific plate), the China continent shows complex regional metallogenic features due to tectonic evolution of “micro-plates, polycycle tectonic movements”. Well developed superimposed metallogenic systems have constituted one of the regional metallogenic features in China. Through the study on superimposed metallogenic system of the middle and lower reaches of the Yangtze River and of the Yuebei basin (northern Guangdong Province), the authors put forward some basic combination pattern of sedimentary-magmatic superimposed metallogenic system and summarize its forming conditions (controlling factors).

关 键 词：metallogenic system SUPERIMPOSITION middle and lower reaches of the Yangtze River Yuebei basin. 

分 类 号：P533[天文地球—古生物学与地层学] P512.2[天文地球—地质学]