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河南省栾川福家村钼多金属矿床地质特征及成矿机理
引用本文:李海森,王喜凤.河南省栾川福家村钼多金属矿床地质特征及成矿机理[J].矿产与地质,2010,24(4):332-337.
作者姓名:李海森  王喜凤
作者单位:河南省有色金属地质矿产局第五地质大队,河南郑州450042
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。

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

The geologic characteristics and metallogenic mechanism of Mo-polymetal deposit in Fujiacun, Luanchuan, Henan province
LI Hai-sen,WANG Xi-feng.The geologic characteristics and metallogenic mechanism of Mo-polymetal deposit in Fujiacun, Luanchuan, Henan province[J].Mineral Resources and Geology,2010,24(4):332-337.
Authors:LI Hai-sen  WANG Xi-feng
Institution:(The fifth geologic group of Henan Provincial Non-ferrous Metals Geological and Mineral Resources Bureau)
Abstract: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
Keywords:Mo-polymetal deposit  geologic characteristics  metallogenic mechanism  prospecting indicator  Fujiacun  Henan
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