地壳是在形成与形变、建造与改造的矛盾斗争中发展起来的。地下水赋存于地壳之中,也必然会受到两个矛盾方面的制约以及其它自然因素和人为因素的影响。在基岩地区,地下水赋存于岩体、岩层的裂隙、溶穴之中,主要受形变与改造的制约,而在松散沉积物地区,地下水赋存于孔隙之中,主要受形成与建造的制约。然而就形变与形成、改造与建造的关系 The crust was developed in the struggle between the formation and deformation, construction and transformation. Groundwater in the crust, which is also bound to be two contradictory constraints and other natural and human factors. In the bedrock area, groundwater exists in the rock mass and the cracks and cavities in the rock layer, which are mainly controlled by the deformation and alteration. In the loose sediment area, groundwater occurs in the pore space and is mainly affected by formation and construction Restrictions. However, the relationship between deformation and formation, transformation and construction