摘要
汾西矿区奥灰岩溶水属郭庄泉域岩溶水系统,它和整个系统既有密切的水力联系,又有其独特的赋存特征。根据多年勘探资料和郭庄泉的研究成果,探讨了矿区内奥灰岩溶水的赋存特征,并结合构造分布和水文地质规律,分析了岩溶水的富集和运移特性,初步总结了奥灰水在本矿区的分布规律。
Karst ground water of Ordovician limestone in Fenxi mining area belongs to K arst ground water system of Guozhuang sprin g field,it has close hydraulic relation wit h whole system,but also there are special p reservative feature.Based on the prospecti ng informations and research achievements of Guozhuang spring for many years,probed i nto preservative feature of Karst ground wa ter of Ordovician limestone in mining area, and analysed richen and move properties of Karst ground water combine with structural distribution and hydrogeological law,and p reliminarily sum up distributive law of Kar st ground water of Ordovician limestone in the mining area.
出处
《中国煤田地质》
2002年第4期31-32,35,共3页
Coal Geology of China
关键词
奥灰水
赋存特征
分布规律
汾西矿区
水文地质条件
霍西煤田
Karst ground water of Ordovician limestone
preservative feature
distribu tive law
Fenxi mining area