布尔津盆地西部凹陷铀成矿水文地球化学条件初探  

Discussion on hydrogeochemical conditions for uranium ore-formation in western sag of Burqin basin

作　　者：陈贤春 成海 

机构地区：[1]中国核工业地质局290研究所,广东韶关512026

出　　处：《铀矿地质》2002年第3期168-173,共6页Uranium Geology

摘　　要：根据水成铀矿床理论 ,本文在论述布尔津盆地水动力及水化学特征的基础上 ,通过资料综合整理 ,着重分析西部凹陷第三系层间水的铀水迁移分带规律 。Based on the metallogenic theory of hydrogenic uranium deposits,and the description of hydrodynamic and hydrochemical characteristics of Burqin basin,as well as the synthesis of existing materials,this paper analyses the migration and zonation of uranium-bearing water in Tertiary interlayer artesian water in the western sag,Burqin basin,and preliminarily discusses the hydrogeochemical conditions for the formation of interlayer oxidation zone sandstone-type uranium deposits.

关 键 词：布尔津西部凹陷 层间氧化带 水文地球化学 

分 类 号：P641.3[天文地球—地质矿产勘探]