河南省栾川福家村钼多金属矿床地质特征及成矿机理  

The geologic characteristics and metallogenic mechanism of Mo-polymetal deposit in Fujiacun,Luanchuan,Henan province

作　　者：李海森 王喜凤 

机构地区：[1]河南省有色金属地质矿产局第五地质大队,河南郑州450042

出　　处：《矿产与地质》2010年第4期332-337,共6页Mineral Resources and Geology

摘　　要：文章对栾川福家村钼多金属矿床的成矿地质背景、矿区及矿床地质特征进行了综合分析,初步探讨了矿床成因机理。研究认为,矿床成因属与燕山期岩浆活动密切相关的高温-中低温热液型钼铜铅锌铁多金属矿床,提出了该区主要找矿标志和找矿方向。The article analyzes Mo-polymetal deposit＇s mineralization geologic background,mining area and ore deposit geologic characteristics,and discusses ore deposit forming mechanism in Fujiacun,Luchuan.The study result shows that the deposit is a molybdenum;copper;zinc;iron polymetal hydrothermal deposit of high-moderate-low temperature which is closely related to Yanshannian magmatic activities.The study proposes main prospecting indicator and direction

关 键 词：钼多金属矿床 地质特征 成矿机理 找矿标志 福家村 河南 

分 类 号：P618.65[天文地球—矿床学]