阿苏达铀矿床水文地质条件分析  

ANALYSIS OF THE HYDROGEOLOGICAL CONDITION IN ASUDA URANIUM DEPOSIT

作　　者：王成渭[1] 岳淑娟[1] 

机构地区：[1]核工业216大队,新疆乌鲁木齐830011

出　　处：《甘肃地质》2007年第4期77-80,共4页Gansu Geology

摘　　要：本文以地质条件为基础,从含水层(带)特征、地下水动态及动、静储量变化、坑道涌水量预测、矿床充水因素、工程地质条件等5个方面对阿苏达铀矿床的水文地质条件进行了分析,确定该矿床属于水文地质条件及工程地质条件简单类型,并对矿山建设及开采提出了建议。Based on the hydrogeological condition, the hydrogeological characteristics of the uranium deposit are analysed in the five aspects as aquifers and its characteristics, the reasons of deposit water filling, groundwater dynamic and dynamic or static state of reserves variation, prediction of tunnel water gushing, engineering geological condition. In this paper the deposit is identified as the simple type of engineering geological condition and some suggestions about construction and exploitation of the mine has been put forward.

关 键 词：铀矿床 水文地质条件 工程地质条件 坑道开采 阿苏达 

分 类 号：P641.4[天文地球—地质矿产勘探] P619.14[天文地球—地质学]