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井孔水位可以较灵敏地反映出地壳应力-应变动态的问题,已被大量的事实所证实,引起了地震、地质、地球物理与水文地质工作者的越来越大的注意,这可能为监测现代地壳活动和地震预报提供出某种途径。然而,对井孔水位反映地壳应力-应变动态的机理研究,至今仍然是一个十分薄弱的领域。单从地震地下水位观测井网得到的资料中进行研究,常常遇到两大困难,一是力源的特征不清楚,二是作为响应机构的井孔——含水层
The wellbore water level can reflect the crustal stress-strain dynamics more sensitively and has been proved by a large number of facts, which has attracted more and more attentions from the earthquake, geology, geophysical and hydrogeological workers. This may be the result of monitoring Modern crustal activity and earthquake prediction provide some way. However, studying the mechanism of borehole stress-strain dynamics in the crust is still a very weak area. The study of single data from seismic well table observation wells often encountered two major difficulties. First, the characteristics of the source were unclear. The second was the wellbore-aquifer