%0 Journal Article
%T 岩脉发育区构造裂隙水勘查研究—以唐县史家佐村地下水勘查为例
%A 刘 蕴
%A 曹 红
%A 朱庆俊
%A 李 伟
%A 王新峰
%A 邓启军
%J 南水北调与水利科技
%D 2013
%X 保定西部太行山区广泛发育强透水岩层、低阻岩脉和富水构造。在该地区寻找构造裂隙水时，关键在于准确区分低阻岩脉（体）与富水断层。利用水文地质调查和物探勘查相结合的方法，通过对比分析低阻岩脉与富水断层的电性差异，成功实施了一眼构造裂隙水勘查示范井。取得了岩脉区寻找构造裂隙水的有效方法，解决了当地多年缺水问题。  A large number of permeable rocks, low-resistance veins, and water-rich structures occur in the Taihang mountains area of western Baoding. To explore the structural fissure water in this area, the key is to how to distinguish the low-resistance veins from water-rich fault accurately. Based on the hydrogeological conditions survey and geophysical exploration, a demonstration well of structural fissure water was successfully implemented through the comparative analysis of the electrical difference between low-resistance veins and water-rich fault. Therefore, the methods to find structural fissure water in the vein developing area was obtained, which solved the water shortage problem in this area  国家自然科学基金项目（41240021）
%K 低阻岩脉
%K 富水断层
%K 构造裂隙水
%K 物探勘查
%K low-resistance veins
%K Wwater-rich fault
%K Sstructural fissure water
%K Ggeophysical exploration
%U http://www.nsbdqk.net/nsbdyslkj/article/abstract/20130522?st=article_issue