断裂找水在豫北山区的应用  

On Water-finding in the Faulted Zone of the Mountains in Northern Henan Province

作　　者：兰自亭[1] 刘玉忠[1] 

机构地区：[1]河南省地质矿产勘查开发局第一水文地质工程地质队,新乡453002

出　　处：《地质调查与研究》2005年第2期120-123,共4页Geological Survey and Research

基　　金：原地矿部定向科研基金项目:河南省缺水山区找水方法研究

摘　　要：以构造控水理论为基础,系统分析理论为指导,运用水文地质调查与综合物理探矿相结合的方法,对缺水严重的豫北山区碳酸盐岩地区基岩地下水进行了找水探讨。受断裂构造的影响,地下水的形成、运移和富集具有一定的规律性。断裂旁侧富水,断裂带富水,断裂交汇部位片状富水,这些都是找水打井的有利地段。通过水文地质调查和水文物探,查明区域地下水位以及含水岩组的埋藏条件,进而确定井位和井深。Based on the theory that faults control water, through the method of hydro-geological survey and the comprehensive geophysical prospecting, the research of water-finding has been worked in the lime stone mountains of northern Henan Province, where the water is badly lack. The formation, movement and enrichment of groundwater effected by the faulted zone follow some rules. The water can get rich at the sides of a fault, in the faulted zones and the intersection of the faults. And these are good places of drilling for searching water. The groundwater level and the burying condition of the aquifers must be found out firstly, and then the place and depth of the wells can be fixed.

关 键 词：豫北山区 断裂 富水地段 岩溶裂隙 

分 类 号：P641.7[天文地球—地质矿产勘探]