依据半弹性空间地震位错理论获得的静应力变化量，可以长期存在于邻近断层面上，直至下一次地震发生。
The changes on static stress, acquired according to the half-space elastic dislocation theory, can exist on fault plane for a long time until the next strong earthquake.
把不确定性引入“时间可预报模式”，可将一次地震之后的平静时间表示成与这次地震位错量大小呈正相关的随机变量。
Introducing indetermination into "time-predictable model", quiet time following an earthquake can be expressed as a random variable which is in positive correlation to the earthquake displacement.
研究结果表明，在使用大地测量资料进行地震位错模型参数反演时，考虑大地水准面形变不仅在理论上更加严格，而且在实际应用中也确有意义。
The results indicate that based on geodetic data inversion of source parameters of earthquake dislocation model is not only theoretically serious, but also practically significant.
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