摘要
内蒙准格尔旗东部地区,广布寒武——奥陶系碳酸盐岩地层,岩溶较为发育,是我国北方岩溶水文地质特征的代表性地区之一。区内属中、低山及丘陵地貌景观。地下水埋藏深,富水性差,人、畜吃水困难,仅在局部地带岩溶水量丰富,水质较好,可作为开发矿区供水水源。因此,研究该区的岩溶发育规律及岩溶水的地质特征,将具有一定的实际和理论意义。
Karst formations are well developed in the Cambrian-Ordovician carbonate strata widely distributed in eastern Zhungeer Banner. The area consists of medium-low mountains and hills , which are one of the typical areas of karst hydrogeology in north China.
Although ground water in the area is mainly deeply buried, poor water -yield propertys and insufficient to supply,karst water in some places is rich in quantity and good in guality,which can be served as sources of water-supply for mine exploitation.
出处
《中国岩溶》
CAS
CSCD
北大核心
1991年第2期108-115,共8页
Carsologica Sinica
关键词
岩溶
水文地质
准格尔旗
Aquifer, Karst fissure, Water-controlled structure, Regularity of water occurrence,Karst landscape
