阶地丘岗中地下水资源的赋存,主要是受新构造的控制。新生代松散含水层中的孔隙水大多分布在新构造断裂的俯侧和带状的地堑中。新生代以前坚硬岩石中的裂隙水主要赋存在张扭性的新构造裂隙径流带内。因此,必须根据赋存条件合理开发利用,同时,要注意环境保护。 The occurrence of groundwater resources in terrace mound is mainly controlled by the new structure. Most of the pore water in the Cenozoic loose aquifers is distributed in the topside and belt-shaped graben of the neotectonic faults. The fissure water in the hard rock before the Cenozoic mainly exists in the neotectonic fissure runoff zone with tensile and torsional properties. Therefore, we must develop and utilize it rationally according to the conditions of occurrence, meanwhile, pay attention to environmental protection.