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民乐山前平原新构造运动十分活跃 ,新第三纪以来的断裂构造 ,造成了盆地基底形态变化 ,从而导致区内地下水位由南向北随断裂带的分布 ,形成了多级跌水陡坎。断层上盘水位埋深一般在 10 0m左右 ,断层下盘水位埋深大于 150m。进一步查明区内基底构造 ,对寻找利于开采的浅埋地下水有着重要的指导意义
The Neotectonic movement in Minle Piedmont Plain is very active. Since the Neogene, the fault structure has resulted in the change of basement morphology of the basin, resulting in the distribution of groundwater table from south to north along the fault zone, forming a multi-level slump ridge . The depth of the fault plate water level is generally about 10 0m, the depth of fault under the water level is greater than 150m. To further ascertain the basement structure in the area has an important guiding significance for finding shallow groundwater that is beneficial to exploitation