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华家岭北麓地质构造条件复杂,主要控水构造为华家岭—暖泉大断裂,该断裂由一系列NW向雁行排列的逆断层组成。受断裂的影响,断裂带内岩石的裂隙、溶隙非常发育,为地下水的储存和运移提供了良好的空间。本文利用取得的勘查资料,对赋存于断裂带内的岩溶水及基岩裂隙水形成的地质背景、水文地质特征等进行了分析。
The geological structure of the northern foot of Huajialing is complex. The main water control structure is the Huazhailing-Nuanquan large fault, which is composed of a series of reverse faults arranged in NW-trending geese. Affected by the fractures, the fractures and sags of the rocks in the fault zone are well developed, which provides a good space for the storage and migration of groundwater. Based on the exploration data obtained in this paper, the geological background and hydrogeological features of karst water and fissure water in bedrock formed in the fault zone are analyzed.