地质构造对韩城矿区水文地质特征的影响  

The effect of geology structure on hydrogeology characteristics of Hancheng mining area

作　　者：代革联[1] 

机构地区：[1]西安科技大学,西安710054

出　　处：《干旱区资源与环境》2010年第7期62-67,共6页Journal of Arid Land Resources and Environment

基　　金：国家自然科学基金(40472104);西安科技大学培育基金(A515010)资助

摘　　要：在分析韩城矿区水文地质条件的基础上,着重讨论了地质构造对韩城矿区水文地质边界、水文地质单元划分、井下突水、岩溶发育和地下水的补给、径流、排泄条件的影响;认为地质构造对地下水的空间分布、形成和运移起着关键性的作用,对水文地质特征的控制作用明显。Based on the analysis of hydrogeology condition of Hancheng mining area,this text emphasized the effect and control of its hydrological boundary,hydrological unit division,underground water inrush,karst development and the recharge,runoff,discharge of groundwater on geology structure.It is considered that hydrogeology characteristics plays a key role in spatial distribution,formation,and moving of the underground water.Hydrogeology characteristics are controlled by geology structure at the great degree.

关 键 词：地质构造 水文地质 特征 边界 岩溶 韩城 

分 类 号：TD163[矿业工程—矿山地质测量]