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湖南衡南杨林坳钨矿床成因与成矿模式研究
引用本文:郑平,徐海珍,黄满湘.湖南衡南杨林坳钨矿床成因与成矿模式研究[J].矿产与地质,2007,21(2):126-130.
作者姓名:郑平  徐海珍  黄满湘
作者单位:中南大学地学与环境工程学院,湖南,长沙,410083
摘    要:以衡南杨林坳钨矿床为研究对象,在对该矿区进行深入的综合地质调查与研究的基础上,从成矿物质来源、成矿过程等方面对其成因进行了系统的研究。结果认为,该矿床属岩浆期后高—中温热液充填-交代型钨矿床,并根据矿床成因建立了相应的成矿模式。

关 键 词:钨矿床  矿床成因  综合地质调查与研究  充填-交代  成矿模式  杨林坳
文章编号:1001-5663(2007)02-0126-05
收稿时间:2007-01-09
修稿时间:2007-01-09

Studies on the genesis and metallogenic model of Yanglin'ao tungsten deposit,Hengnan,Hunan province
ZHENG Ping,XU Hai-zhen,HUANG Man-xiang.Studies on the genesis and metallogenic model of Yanglin''''ao tungsten deposit,Hengnan,Hunan province[J].Mineral Resources and Geology,2007,21(2):126-130.
Authors:ZHENG Ping  XU Hai-zhen  HUANG Man-xiang
Institution:School of Geoscience and Environmental Engineering,Central South University,Changsha 410083 ,China
Abstract:Through intensive studies and surveys on the geology of the Yanglin'ao Tungsten Deposit(YTD),and from such factors as the source of ore-forming material and mineralized process,the author made systematical analyses on the deposit genesis and concluded that YTD is a postmagmatic hyper-mesothermal filled metasomatic deposit.In this paper a metallogic model is also put forward on the basis of the deposit genesis.
Keywords:tungsten deposit  deposit genesis  miscellaneous geologic investigations  filled metasomatic  metallogenic model  Yanglin'ao
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