湖南邓阜仙地区成矿条件及找矿方向  

Ore-forming Conditions and Range of Reconnaissance for Polymetallic Deposits in Dengfuxian, Hunan

作　　者：蔡维[1] 朱浩锋[1] 郭锦[1] 李兆宏[1] 

机构地区：[1]湖南省地质矿产勘查开发局四一六队,湖南株洲412007

出　　处：《四川地质学报》2014年第4期538-542,共5页Acta Geologica Sichuan

基　　金：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。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.

关 键 词：有色多金属 成矿条件 找矿 邓阜仙地区 

分 类 号：P618.4[天文地球—矿床学]