内蒙古阴山山脉中段地质构造演化及成矿期划分  

Tectonic Evolution And Metallogenic Period Division Of Yinshan Middle Range In Inner Mongolia

作　　者：李辰 LI Chen(Guozhen Environmental Remediation,Hefei 230000,China)

机构地区：[1]安徽国祯环境修复股份有限公司,安徽合肥230000

出　　处：《世界有色金属》2022年第15期88-90,共3页World Nonferrous Metals

摘　　要：研究区位于华北地台北缘阴山山脉中段。研究区中部为色尔腾山,北侧为渣尔泰山,南侧为乌拉山、东侧为大青山,该区域矿产资源丰富,开展地质调查研究价值高。从20世纪60年代起,国内多个地质单位对该地区进行了地质调查工作,但多数工作重点突出在该地区的色尔腾山群和渣尔泰山群的地层研究,或是基于对该区域岩浆岩成因研究,未对该地区进行全面的构造演化研究。本文则通过对前人的研究成果进行归纳总结,全面梳理了研究区的地质演化过程,以及对应的成矿期次划分,为后期在研究区开展地质研究及找矿工作提供依据。The research area is located in the middle of Yinshan Mountain range on the edge of the North China Platform.The central part of the study area is Serteng Mountain.The north side is Jer Tai Mountain.The south side is Wula Mountain,and the east side is Daqingshan mountain.This area is rich in mineral resources and has high value for geological investigation and research.Since 1960s,many domestic geological units have carried out geological survey in this area,but most of the work focuses on the stratigraphy research of sertengshan group and Jargtai Group in this area,or based on the study of the genesis of magmatic rocks in this area,there is no comprehensive study on the tectonic evolution of this area.This paper summarizes the previous research results,comprehensively combs the geological evolution process of the study area,and the corresponding metallogenic period division,and provides a basis for the later geological research and prospecting work in the study area.

关 键 词：阴山山脉中段 构造演化 成矿期 

分 类 号：P618.4[天文地球—矿床学]