桂北某矿田地球物理地球化学场特征及其与深部成矿的关系探讨  

Geophysical and geochemical field characteristics in an ore fieldin northern Guangxi and its relationship with deep mineralization

作　　者：郑可志 ZHENG Kezhi(No.310 Geology Party of Nuclear Industry,Guangxi Zhuang Autonomous Region,Guilin 541213,Guangxi,China)

机构地区：[1]广西壮族自治区三一〇核地质大队,广西桂林541213

出　　处：《资源信息与工程》2023年第2期5-8,共4页Resource Information and Engineering

摘　　要：本文在综合分析研究前人成果资料的基础上,总结桂北某矿田地球物理地球化学场特征,指出区域上的相对伽马偏高场反映了铀元素相对富集,对寻找地表及浅部矿体有指示作用;氡及其子体、210Po测量成果对深部找矿有指示作用。On the basis of comprehensive analysis and study of previous achievements,this paper summarized the geophysical and geochemical field characteristics in an ore field in northern Guangxi,and pointed out that the relative gamma high field in the region reflects the relative enrichment of uranium elements,indicating the surface and shallow ore bodies;Radon and its daughters,210 Po survey results are indicative for deep ore prospecting.

关 键 词：地球物理场 地球化学场 深部成矿 

分 类 号：P618.51[天文地球—矿床学]