摘要
通过对津巴布韦某金矿成矿远景区开展1∶10000土壤化探工作,结果表明:Au的相对高异常区主要分布在花岗岩与石英脉接触带或破碎带附近,其高值从形态展布上受近EW向构造控制。分析结果为下一步工程布置提供了参考依据。
Through 1∶10000 soil geochemical exploration on a gold metallogenic prospective area in Zimbabwe,the result show that the relatively high anomaly area of gold is mainly distributed near the contact zone or fracture zone of granite and quartz veins.It is controlled by the EW structure,which provide reference for the next project layout.
作者
江伟华
Jiang Weihua(China Non-Metallic Minerals Industry Association)
出处
《现代矿业》
CAS
2020年第8期22-23,共2页
Modern Mining
关键词
金矿
成矿远景区
土壤化探
Gold deposit
Metallogenic prospective area
Soil geochemical exploration