柬埔寨柏威夏省龙山金矿地质特征及其成矿分析

    Analysis of Longshan gold mine geological characteristic and its origin in Preah-Vihear,the Kingdom of Cambodia

    • 摘要: 为落实“一带一路”矿产资源重大战略,更好地引导我国企业在柬埔寨实现地质找矿重大突破,通过对柬埔寨柏威夏省龙山金矿的野外地质调查、样品测试以及资料梳理,初步剖析了该矿区位于墨江-黎府-罗文真火山弧成矿亚带,受印支燕山期岩浆喷发侵入强烈,矿体产于中酸性闪长岩和花岗闪长岩等,且受罗文真穹窿压扭性断裂构造控制,呈脉状、囊状;赋矿围岩蚀变主要为黄铁矿化、硅化和绢云母化等。该矿床具有位于火山弧带,埋藏浅、品位高等特征,初步判断为火山热液充填交代石英脉型金矿。成矿主要划分为石英-黄铁矿阶段,石英-硫化物阶段和碳酸盐化阶段三个阶段。

       

      Abstract: To implement the important mineral resources strategy “Belt and Road”,also leading Chinese enterprises to achieve brilliant geological outcomes in the Kingdom of Cambodia,the Longshan gold deposit in Preah-Vihear Province of Cambodia have been investigated in field geology,sample testing and indoor information analysis.The preliminary analysis has been taken that the mining area located in Mojiang-Lifu-Luo wenzhun volcano arc metallogenic belt.It’s strongly erupted by magmatic in Indosinian and Yanshan period.The ore body occurs in intermediate-acidic diorite and granodiorite.Those are mainly controlled in vein and saccate by compressive torsional structure in Luowenzhen fornix.The wall rock alteration is mainly pyritization,silicification and sericitization,etc.This gold deposit is namely Volcanic Hydrothermal Filling Alteration of quartz vein type,because of the ore deposit is characteristics of located in the volcano arc zone,shallow buried depth and high grade,etc..Therefore,it is mainly divided into three stages which are quartz pyrite,quartz sulfide and carbonate.

       

    /

    返回文章
    返回