摘要
根据娘子关泉群系统西部控水构造、含水层段、水动力场等水文地质条件,重新划定了娘子关岩溶水系统西部边界(兴道—大方山—郭家沟一线构造带),则东山区成为娘子关的一个补给径流区。在此基础上,对西部子系统岩溶水径流特征提出了新的见解。
According to hydrogeological conditions of water control structure,aquifer and hydrodynamic field,the western bor-der(Xingdao-Dafangshan-Zhaidao structural belt)of Niangziguan karst water system was re defined.Thus the Dongshan Area has found one of runoff source area of Niangziguan springs.On this basis,a new understanding of western subsystem karst water runoff features was advanced.
出处
《中国煤田地质》
2003年第5期26-28,共3页
Coal Geology of China
关键词
岩溶水系统
西部子系统
径流特征
娘子关泉群
karst water system
western subsystem
runoff feature
Niangziguan springs
