摘要
狼牙山断块位于太行山东麓,是一缺水山区。组成地层为白云岩、石灰岩和灰岩与页岩互层;裂隙发育,但溶蚀程度不一。多年来曾利用航片,根据光迹线包括断裂线、破裂迹和节理迹构成的网络找寻岩溶裂隙水,选择了大量井位,获得良好效果。
The fault blocked Layasha moutai is situated at the cast foot of Mout Taihag, where is a arca deficiet of water. The stratigraphy cosists of dolomite, limestoe ad iterbeddig of limestoe ad shale. They are developed i fractures ad vary i solubility. Durig the recet gears, good results have bee achicvcd i well-poit locatig ad karst-fractured groudwater prospectig usig acrial-photos. These are based o etworks of photo-lieamets icludig lieamets, fractures, ad traces of joits.
出处
《勘察科学技术》
1989年第1期27-32,共6页
Site Investigation Science and Technology