水口山矿田康家湾铅锌金银矿区地质特征及探采对比分析

Geological characteristics and exploration and mining comparative analysis of Kangjiawan lead zinc gold and silver mining area in Shuikoushan mine field

水口山矿区地处南岭成矿带中部,邵阳~郴州北西向深断裂带北侧,株洲~江永北东向深断裂与耒阳~临武南北向构造带的交汇部位,上地幔隆起区(衡阳断陷盆地)南缘,该区深部有羊角塘~水口山~五峰仙东西向壳断层,衡东~水口山~江永北东向断裂和水口山~香花岭南北向基底断裂交汇于此,共同控制着深部壳、幔混源岩浆及矿田中铅锌铜金银矿床的产出部位,本文对水口山矿田康家湾铅锌金银矿区地质特征及探采对比分析。

Shuikoushan Mining Area is located in the middle of Nanling metallogenic belt,the north side of Shaoyang Chenzhou North West deep fault belt,the intersection of Zhuzhou Jiangyong North East deep fault and Leiyang Linwu North South structural belt,the south edge of the upper mantle uplift area(Hengyang fault basin),the deep part of which is yangjiaotang Shuikoushan wufengxian East West crust fault,Hengdong Shuikoushan Jiangyong North East fault And Shuikoushan Xianghualing south to North basement fault intersect here,jointly controlling the deep crust,mantle mixed magma and the occurrence of lead zinc copper gold and silver deposits in the ore field.This paper analyzes the geological characteristics and exploration and mining comparison of Kangjiawan lead zinc gold and silver deposit in Shuikoushan ore field.