摘要
金盆金矿位于湖南“金腰带”上的浏阳—醴陵地区金成矿带上,在区域上属于浏阳—衡东隆起带中段与北西向的长沙—萍乡大断裂的复合部位。根据矿区矿(化)体产出现状,表现出沿花岗闪长岩向中深部延深的特征。本文对矿区地质背景和矿床地质特征进行了分析,探讨了主要找矿标志和找矿方向,指出花岗闪长岩是矿区下一步找矿的有利区段。
The gold deposit is located in the Golden Belt of Liuyang Liling area on the“golden belt”of Hunan Province,and belongs to the compound part of the middle part of the Liuyang—Hengdong County uplift belt and the NW trending Changsha Pingxiang fault.According to the present occurrence of ore bodies in the mining area,it shows that the ore bodies extend along the middle and deep part of the Granodiorite,indicating that the granodiorite is the favorable section for further prospecting in the mining area and the direction for further prospecting in the mining area.
作者
谈治林
TAN Zhi-lin(No.214 Geological Party,Hunan Geological&Mining Organization for Non Ferrous Metals,Zhuzhou 412007,Hunan,China)
出处
《资源信息与工程》
2020年第2期27-29,35,共4页
Resource Information and Engineering
关键词
金盆金矿
地质特征
找矿标志
找矿方向
Jinpan gold deposits
geological characteristics
prospecting marks
prospecting direction