壳幔边界复杂性的差异为强震的孕育提供了深部环境。
The difference of crust-mantle complexity provides deep background for the development of strong earthquake.
这两个时间段的出现时间与未来强震的震级呈一定线性关系。
There is some linear correlation between appearing time of the time stages and the magnitude of future strong earthquake.
地震学家所能做的，只是找出那些未来发生强震的可能性很大的地方。
What seismologists can do is identify places where there is a high probability of a strong earthquake happening in the future.
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