摘要
基于区域水文地质条件,论述了新疆十三师镜儿泉钼矿的水文地质特征。研究表明,研究区地下水类型主要包括基岩裂隙水、碎屑岩类孔隙裂隙水和松散岩类孔隙水等三种类型。地下水来源于主要为南部山区的地下水侧向径流补给,排泄以浅埋带蒸发、侧向径流、人工开采为主。研究成果为矿区矿产资源的开发和利用提供了依据。
This paper deals with regional hydrogeological characteristics of the Jingerquan Mo deposit in Xinjiang. The study indicates that underground water may be divided into 3 types such as bedrock fissure water, clastic rock pore fissure water and loose rock pore water. The underground water is originated from mountains in the south with lateral flow supply. Underground water discharge is evaporation in shallow buried zone, lateral flow and artificial exploitation.
出处
《四川地质学报》
2017年第1期124-127,共4页
Acta Geologica Sichuan
关键词
钼矿
地下水
地质条件
镜儿泉
Mo deposit
underground water
geological condition
Jinger Spring
