而水位异常图像出现的上升或下降形态，取决于井孔含水层系统在大震孕育过程的应力调整再积累阶段所处的构造部位。
However, decline or rise of water level anomaly depends on the tectonic position where the well aquifer lies in the process of stress regulation and re accumulation.
又由于井孔-含水层系统、距海远近和江河湖海水力联系等条件的差异而表现出多种多样的水位动态。
The various dynamic state of the water levels are due to different distance of water well from the coast and different hydraulic relation among the river, the lake...
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