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枣庄地区属于华北台块鲁西南台背斜南部,是暴露和半暴露的缓倾斜以构造断裂为主的构造中常地区。含水岩层以坚硬岩石裂隙岩溶水为主,主要含水层有寒武纪灰岩、奥陶纪灰岩、石炭纪薄层灰岩及侏罗纪砾岩。这些坚硬岩石由于含水性能的不均一性,其富水程度及地下径流条件即同一地区同一含水层中差异亦很大,如果忽视这种差异的复杂性,往往会使开采和防治地下水不能达到
The Zaozhuang area belongs to the southern part of Luxi South Taiwan anticline in the North China block. It is a moderately exposed tectonogene in the gently exposed and semi-exposed tectonic faults. The aquifer is dominated by hard rock fractured karst water. The main aquifers are Cambrian limestone, Ordovician limestone, Carboniferous thin layer limestone and Jurassic conglomerate. Due to the heterogeneity of water-bearing properties, these hard rocks have different water-rich degree and subsurface flow conditions, namely, the same aquifer in the same area. If the complexity of this difference is neglected, the exploitation and prevention of groundwater can not be achieved