承德地区铁矿类型及其地质特征  

Types and Geological Characteristics of the Iron Deposits in Chengde

作　　者：郭静粉[1] 张立剑[1] 

机构地区：[1]河北省地质矿产勘查开发局第四地质大队,河北承德067000

出　　处：《中国锰业》2016年第5期35-37,共3页China Manganese Industry

摘　　要：在分析了承德地区铁矿资源总体特征的基础上,对承德地区铁矿按成因类型进行了分类,包括岩浆型、沉积变质型、接触交代型、火山热液型和沉积型五类。对不同成因类型矿床的成矿地质背景、控矿条件进行了分析,叙述了典型矿床的矿体特征、矿石质量、矿石类型等,并总结了各类型铁矿的特点。Based on the analysis of the characteristics of Iron resources in Chengde,iron deposits are classified into 5 genetic types： magmatic type, metamorphosed sedimentary type, skarn type, volcanic hydrothermal type and sedimentary type. This paper .analyzed the metallogenic geological setting and controlling conditions of different genetic types of ore deposits. It described the characteristics of ore bodies, ore quality and types of ore deposits. At last, it summarized the characteristics of each type of iron deposits in Chengde.

关 键 词：承德 铁矿 成因类型 成矿地质背景 矿体特征 

分 类 号：P618.31[天文地球—矿床学]