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地震经常在其他断层上诱发余震,但其机理依然难以确定。一种创新的分析使我们获得关于由地震波通过引起动应力效应的新认识。
Earthquakes often induce aftershocks on other faults, but the mechanism remains uncertain. An innovative analysis allows us to gain a new understanding of the effect of dynamic stress induced by seismic waves.