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湖南邓阜仙地区成矿条件及找矿方向
引用本文:蔡维,朱浩锋,郭锦,李兆宏.湖南邓阜仙地区成矿条件及找矿方向[J].四川地质学报,2014(4):538-542.
作者姓名:蔡维  朱浩锋  郭锦  李兆宏
作者单位:湖南省地质矿产勘查开发局四一六队,湖南株洲412007
基金项目:国土资源部公益性行业科研专项“湖南锡田地区钨锡矿成矿规律及靶区预测研究”(201211024); 地质矿产调查评价专项项目“湖南茶陵太和仙-鸡冠石锡多金属矿远景调查”(1212011085376).
摘    要:湖南邓阜仙地区位于南岭钨锡铅锌多金属成矿带湖南段东部北侧,郴州—茶陵北东向钨锡多金属成矿区带北东段北侧。研究从区内地层、构造、岩浆活动入手。总结出岩浆和围岩地层是该区的成矿物质来源,而构造则形成了矿液通道与赋矿空间。最后,在以上研究的基础上,指出下一步该区主要是寻找裂隙型、矽卡岩型和隐伏型矿床。

关 键 词:有色多金属  成矿条件  找矿  邓阜仙地区

Ore-forming Conditions and Range of Reconnaissance for Polymetallic Deposits in Dengfuxian,Hunan
CAI Wei,ZHU Hao-feng,GUO Jin,LI Zhao-hong.Ore-forming Conditions and Range of Reconnaissance for Polymetallic Deposits in Dengfuxian,Hunan[J].Acta Geologica Sichuan,2014(4):538-542.
Authors:CAI Wei  ZHU Hao-feng  GUO Jin  LI Zhao-hong
Institution:(No. 416 Geological Team, Bureau of Geology and Mineral Exploration and Development of Hunan Province, Zhuzhou, Hunan 412007)
Abstract:The Dengfuxian area is located in the east Hunan section of the Nanling tungsten-tin-lead-zinc polymetallic metallogenic belt and in the Northeast section of the Chenzhou-Chaling W-Sn polymetallic metallogenic belt. This paper believes that the ore material was derived from strata as wall rocks and ore-formation was controlled by fracture. Crevice and skarn type of deposits are of perspective.
Keywords:range of reconnaissance  magmatite  structure  Dngfuxian area
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