山西省关沟地区沉积变质铁矿地质特征分析  

The geological characteristics of sedimentary metamorphic iron mine in Guangou of Shanxi province

作　　者：赵文艳[1] 郗宝华[1] 

机构地区：[1]山西煤炭职业技术学院,山西太原030031

出　　处：《世界有色金属》2015年第10期71-72,共2页World Nonferrous Metals

摘　　要：通过对关沟地区沉积变质铁矿的地质特征、矿层特征以及矿石质量分析,指出该区域的矿床形成过程中地层控矿是内因,区域变质作用以及后期岩浆岩的侵入是外因。Through analysis of sedimentary metamorphic iron mine geological features, ore characteristics and ore quality of Guangou area, pointed out that the deposits in the region of the formation of formations in the process of geosphere controlling is the internal cause, regional metamorphism and magmatic rock intrusion is external.

关 键 词：沉积变质型 铁矿 地质构造 

分 类 号：P618[天文地球—矿床学]