Sarlis Nicholas V, Skordas Efthimios S, Varotsos Panayiotis A, Ramírez-Rojas Alejandro, Flores-Márquez Elsa Leticia
Section of Solid State Physics, Department of Physics, National and Kapodistrian University of Athens, Panepistimiopolis, 157 84 Zografos, Athens, Greece.
Solid Earth Physics Institute, Department of Physics, National and Kapodistrian University of Athens, Panepistimiopolis, 157 84 Zografos, Athens, Greece.
Entropy (Basel). 2019 Mar 20;21(3):301. doi: 10.3390/e21030301.
It has been shown that some dynamic features hidden in the time series of complex systems can be unveiled if we analyze them in a time domain termed natural time. In this analysis, we can identify when a system approaches a critical point (dynamic phase transition). Here, based on natural time analysis, which enables the introduction of an order parameter for seismicity, we discuss a procedure through which we could achieve the identification of the occurrence time of the M8.2 earthquake that occurred on 7 September 2017 in Mexico in Chiapas region, which is the largest magnitude event recorded in Mexico in more than a century. In particular, we first investigated the order parameter fluctuations of seismicity in the entire Mexico and found that, during an almost 30-year period, i.e., from 1 January 1988 until the M8.2 earthquake occurrence, they were minimized around 27 July 2017. From this date, we started computing the variance of seismicity in Chiapas region and found that it approached the critical value 0.070 on 6 September 2017, almost one day before this M8.2 earthquake occurrence.
研究表明,如果我们在一个称为自然时间的时域中对复杂系统的时间序列进行分析,一些隐藏在其中的动态特征就可以被揭示出来。在这种分析中,我们可以确定一个系统何时接近临界点(动态相变)。在此,基于能够引入地震活动性序参量的自然时间分析,我们讨论一种程序,通过该程序我们可以确定2017年9月7日发生在墨西哥恰帕斯州的8.2级地震的发生时间,这是墨西哥一个多世纪以来记录到的震级最大的事件。具体而言,我们首先研究了整个墨西哥地震活动性的序参量波动,发现在近30年的时间里,即从1988年1月1日到8.2级地震发生期间,它们在2017年7月27日左右达到最小值。从这个日期开始,我们开始计算恰帕斯州地震活动性的方差,发现其在2017年9月6日接近临界值0.070,几乎就在这次8.2级地震发生的前一天。