这一信息可帮助计算地震能量释放速度,并以此计算岩层断裂速度。
That allows it to work out how quickly energy was released by the earthquake, and thus how fast the rupture propagated.
岩层断裂引发深震传播速度很快——大约3km/秒。
The rupture in the rock that causes a deep earthquake propagates rapidly—at about 3km a second.
运用这一关系可通过层速度预测断裂的封闭性。
Hence the sealing capacity of faults can be predicted by seismic interval velocity.
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