新疆布尔津盆地砂岩型铀矿成矿水文地质条件初探  

DISCUSSION ON HYDROGEOLOGICAL CONDITIONS OF METALLOGENESIS OF THE SANDSTONE TYPE URANIUM DEPOSIT IN BURQIN BASIN, XINJIANG AUTONOMOUS REGION

作　　者：李启荣 

机构地区：[1]华南地质局,广东韶关512026

出　　处：《铀矿地质》2000年第6期343-352,共10页Uranium Geology

摘　　要：本文在简要介绍布尔津盆地地下水赋存条件与分布的基础上 ,论述了该盆地的构造 水文地质层特征 ,进而着重阐明区内地下水补、径、排等水动力条件以及水文地球化学特征 ,总结了有利的铀矿成矿水文地质条件。Based on a brief introduction to the occurrence and distribution of groundwater, the characteristics of the tectonic hydrogeological layers of the basin are discussed. Then, this paper expounds the groundwater hydrodynamic conditions including recharge, runoff and drainage, and hydrogeochemical characteristics. In the end, the hydrogeological conditions favorable for uranium metallogenesis are summarized.

关 键 词：布尔津盆地 砂岩型铀矿 水文地质条件 成矿环境 

分 类 号：P619.140.5[天文地球—矿床学] P641.463[天文地球—地质学]