荔浦白石山铜矿水系沉积物地球化学特征  

The Unusual Characteristics of Sediment Geochemistry in Outer Water of Baishishan’s Copper mine

作　　者：施玉娇[1] 周奇明[1] 李小兰[1] 史琪[1] 

机构地区：[1]桂林矿产地质研究院,广西桂林541004

出　　处：《大众科技》2012年第1期157-159,共3页Popular Science & Technology

摘　　要：通过对白石山铜矿外围水系沉积物地球化学异常特征的研究,认为该区内具有良好的寻找铜矿的前景,Pb、Zn为近矿指示元素,Cr、V、Co为远程指示元素。文章指出处于背斜核部的NEE向断裂破碎带即为良好的储矿空间,也为良好的导矿通道,为今后找矿的重要靶区。Through the researches to the unusual characteristics of sediment geochemistry in outer water of Baishishan＇s Copper mine, to finding copper has very prospects.Pb and Zn are close indicate elements,but,Cr, V and Co are far indicate elements.In my opinion,The NEE direction＇s fracture zones at the core of the anticline are good ore-space,but also are good guide for the mine tunnel,Cu elements combination unusual areas are most important targets.

关 键 词：铜矿 水系沉积物 地球化学特征 白石山 

分 类 号：P62[天文地球—地质矿产勘探]