首页|湖南湘东邓阜仙矿集区钨锡多金属成矿系统及成矿模式研究

湖南湘东邓阜仙矿集区钨锡多金属成矿系统及成矿模式研究

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邓阜仙矿集区位于湖南省茶陵县东北部,钦杭结合带西南段,南岭成矿带东段,大地构造位置上处于赣南隆起与湘桂坳陷的交接部位.区内矿产资源丰富,发育钨锡、铅锌、铌钽等稀有金属矿床,典型矿床包括湘东钨矿床(又名邓阜仙钨矿床)、金竹垄铌钽矿床、鸡冠石钨矿床、大垄铅锌矿床,太和仙铅锌矿床,均为岩浆期后热液成矿作用成矿,成矿潜力巨大,且形成一个完整的高-中-低温热液成矿系列.通过对该矿集区矿床地质特征、成矿物理化学条件、成矿物质及成矿流体来源、成矿时代、成矿作用及矿床成因等的方面研究,建立该矿集区成矿系统以及成矿模式,指导本地区及同类矿床的边深部找矿有实际意义.
Study on Metallogenic System and Metallogenic Model of Tungsten-Tin Polymetallic Deposit in Dengfuxian Ore Concentrated Area,Eastern Hunan Province
The Dengfuxianore concentrated area in the northeast of ChalingCounty,Hunanprovince,is locatedin the Southwest section of the Qinzhou-Hangzhou Junction,the eastern part of the Nanling metallogenic belt.The tectonic position is at the junction of southern Gannan Uplift and Xiang-gui depression.Mineral resources are abundant in the area,and rare metal deposits such as tungsten,tin,lead,zinc,niobium and tantalum are developed.Typical deposits include Xiangdong tungsten deposit(also known as Dengfuxian tungsten deposit),Jinzhulang niobium-tantalum deposit,Jiguanshi tungsten deposit,Dagang lead-zinc deposit,Taihexian lead-zinc deposit,all of which are post-magmatic hydrothermal mineralization,mineralization potential is huge,and form a complete high-medium-low temperature hydrothermal metallogenic series.Based on the studying the geological characteristics,physical and chemical conditions of the ore deposit,the source of ore-forming material and fluid,the ore-forming age,the ore-forming process and the genesis of the ore deposit,the metallogenic system and metallogenic model of the ore concentration area were established,whichhas the practical significance toguide the deep and side prospecting of the same ore deposit in this area.

Dengfuxian ore concentrated areahigh-medium-low temperature hydrothermal mineralizationmetallogenic systemmetallogenic model

王淑军、陈自文

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湖南省水文地质环境地质调查监测所,长沙 410129

邓阜仙矿集区 高-中-低温热液成矿 成矿系统 成矿模式

2024

四川地质学报
四川省地质学会

四川地质学报

影响因子:0.314
ISSN:1006-0995
年,卷(期):2024.44(1)
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