普安县石寨坪成矿地质特征研究  

Research on Metallogenic Geological Characteristics in Pu′an Shizhaiping

作　　者：杜昌乾[1] 

机构地区：[1]贵州省地质矿产勘查开发局106地质大队,贵州遵义563000

出　　处：《煤炭技术》2017年第11期109-111,共3页Coal Technology

摘　　要：结合成矿区域地质背景,在研究铅锌矿的矿体特征、矿物组分、矿石结构构造及矿物共生组合的基础上,对矿床成因进行了分析,认为区内铅锌矿床为浅成低温热液型铅锌矿床,其形成经历了构造热液成矿期及后生氧化富集阶段。对找矿标志做了深层次探讨,总结了石寨坪铅锌矿找矿标志,这对该区域的铅锌矿勘查、研究有着重要的理论指导意义。Based on structure and mineral the analysis for orebody association, the genesis of background of minerogenetic area. The results characteristics, mineral constituent, ore texture and mineral deposit is analyzed combining with geological show that the Shizhaiping lead-zinc deposit is an epithermal deposits, and its formation has undergone tectonic hydrothermal ore-forming period and epigenetic oxidation enrichment stage. The indicators for deposit are discussed. It plays an important theoretical guiding significance for exploration and research of lead-zinc deposit in the area.

关 键 词：铅锌矿床 地质特征 矿床成因 找矿标志 

分 类 号：P618.4[天文地球—矿床学]