Results of the scaling analysis of the waiting time series for seismic events of the 2019 Ridgecrest earthquake sequence in East California have been presented. It has been shown that the waiting time series before a strong earthquake with a magnitude of M = 7.1 acquires a scale-invariant structure. A reason for the appearance of the statistical self-similarity in the waiting time series is the transition of the medium in the focal region to a strongly nonequilibrium state. The result can be interpreted as the appearance of a temporal dissipative structure in the process of seismic kinetics. It has been proposed to use the scaling analysis of the seismic kinetic data to monitor the current state of the seismogenerating medium.

提出了对东加利福尼亚州2019年Ridgecrest地震序列的地震事件的等待时间序列进行比例分析的结果。研究表明，在M = 7.1级强地震之前的等待时间序列具有尺度不变的结构。在等待时间序列中出现统计自相似性的原因是焦点区域中的介质过渡到强烈的非平衡状态。结果可以解释为地震动力学过程中时间耗散结构的出现。已经提出使用地震动力学数据的标度分析来监视地震发生介质的当前状态。