有人认为这一系列相对来说规模较小的地震是潜没地带为适应04年地震之后形成的应力分布模式自身调节的结果。但是一些研究人员却对此持怀疑态度。

Some researchers say they suspect that the series of somewhat weaker quakes represents the subduction zone readjusting itself to changes in stress patterns established by the '04 quake.

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从断层间相互作用产生的同震库仑应力改变入手，提出了断层间相互作用的触震与缓震效应，探讨了断层间的相互作用对断层活动性、断层未来地震潜势及余震活动分布图像的影响。

Based on the concept of the change in co-seismic Coulomb stress resulting from the interaction of faults, the earthquake trigging and delaying effects of fault interaction are proposed in this paper.

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