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湖南虎形山钨铍多金属矿床地质特征及成因初探
引用本文:唐朝永,陈云华,游先军,刘利生,张强录,晏月平,王开朗,任杰.湖南虎形山钨铍多金属矿床地质特征及成因初探[J].矿产与地质,2013(5):353-362.
作者姓名:唐朝永  陈云华  游先军  刘利生  张强录  晏月平  王开朗  任杰
作者单位:[1]桂林理工大学资源与环境工程学院,广西 桂林541004 [2]湖南省有色地质勘查局二四七队,长沙410129 [3]湖南省有色地质勘查局,长沙410007
基金项目:湖南省国土资源厅地质勘查项目《湖南省临湘市虎形山地区钨多金属矿控矿规律研究》(编号:201003001)资助.
摘    要:虎形山钨铍多金属矿是湘东北地区目前为止最大的一个钨多金属矿床,伴生有铍铜钼等多金属。矿床赋存于寒武系地层中,属于中温热液-构造脉状型矿床,成矿时代为燕山晚期,成矿物质具多源性,主要来自于深部岩浆,同时也有壳源成分的补充。文章通过矿床地质特征的分析,就矿床成因做些初步探讨,希望能为该地区的后续找矿工作起到一点启示作用。

关 键 词:钨铍多金属  矿床地质特征  矿床成因  虎形山  湖南

Geological characteristics and genesis of Huxingshan W-Be polymetallic deposit in Hunan
TANG Chao-yong,CHEN Yun-hua,YOU Xian-jun,LIU Li-sheng,ZHANG Qiang-lu,YAN Yue-ping,WANG Kai-lang,REN Jie.Geological characteristics and genesis of Huxingshan W-Be polymetallic deposit in Hunan[J].Mineral Resources and Geology,2013(5):353-362.
Authors:TANG Chao-yong  CHEN Yun-hua  YOU Xian-jun  LIU Li-sheng  ZHANG Qiang-lu  YAN Yue-ping  WANG Kai-lang  REN Jie
Institution:1. Department of Resources and Environment Engineering, Guilin University of Technology, Guilin 541004, Guangxi , China; 2. No. 247 Team of Hunan Nonferrous Metals Geology and Exploration Bureau, Changsha 410129, China; 3. Hunan Nonferrous Metals Geology and Exploration Bureau, Changsha 410007, China)
Abstract:Associated with beryllium,copper,molybdenum and other metal,Huxingshan W-Be polymetallic deposit is one of the largest W-Be polymetallic deposit in northeast Hunan.The deposit occurs in Cambrian strata,and it is a medium temperature structure-hydrothermal vein type deposit which is formed in late Yan-shanian metallogenic epoch.The metallogenic materials are polygenetic and are mainly generated from deep magma as well as crust-derived material.After analyzing geological characteristics of the deposit,this paper makes some initial conclusions on genesis of the deposit and tries to provide some ideas for further prospec-ting work.
Keywords:W-Be polymetallic  deposit geological characteristics  deposit genesis  Huxingshan  Hunan
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