广西来田矿区矿床成因及找矿标志浅析

Genesis of ore deposits and ore prospecting criteria in Laitian mining area,Guangxi

广西来田矿区地处北西向南丹～昆仑关深断裂带与北东向凭祥～大黎深断裂带交汇处,断裂构造发育,矿床(体)严格受断裂构造控制,矿床类型主要为构造破碎带热液充填型。通过综合分析矿区地质特征等,浅谈一下矿区铅锌、铜矿床的成因及找矿标志。

The Laitian mining area is located at the intersection of the nw-trending Nandan-Kunlun Pass deep fault zone and the nw-trending pingxiang-dalili Deep Fault Zone The main type of the deposit is hydrothermal fluid filling in the tectonically fractured zone. Based on the comprehensive analysis of the geological characteristics of the mining area, this paper discusses the genesis and prospecting criteria of the pb-zn and cu deposits.