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与2017年9月8日墨西哥恰帕斯州近海8.1级地震相关的超低频震前地磁异常信号

ULF Pre-Seismic Geomagnetic Anomalous Signal Related to Mw8.1 Offshore Chiapas Earthquake, Mexico on 8 September 2017.

作者信息

Stănică Dragoș Armand, Stănică Dumitru

机构信息

Department of Electromagnetism and Lithosphere Dynamics, Institute of Geodynamics of the Romanian Academy, R-020032 Bucharest, Romania.

出版信息

Entropy (Basel). 2019 Jan 3;21(1):29. doi: 10.3390/e21010029.

Abstract

In the last decade, the real time ground-based geomagnetic observations realized in correlation with the Vrancea seismicity in Romania, together with supplementary studies related to some earthquakes (Mw9.0 Tohoku, Japan on 11 March 2011 and Mw8.3 Coquimbo, Chile on 16 September 2015), enlarged our knowledge about the relationship between the pre-seismic anomalous phenomena and the final stage of the earthquake nucleation. To identify possible ultra-low-frequency (ULF) geomagnetic signals prior to the onset of an Mw8.1 earthquake, we retroactively analyzed the data collected on the interval 1 August-16 September 2017 at the Geomagnetic Observatories in Teoloyucan (TEO), Mexico and Tucson (TUC) USA, with the last taken as a reference. Daily mean distributions of the polarization parameter BPOL (geomagnetic polarization parameter) and standard deviation are obtained for both observatories using a fast Fourier transform (FFT) band-pass filtering in the ULF range (0.001-0.083 Hz). Further on, we investigated the singularity of the pre-seismic signal associated with an Mw8.1 earthquake and applied a statistical analysis based on a standardized random variable equation; results are presented as BPOL* time series on the interval 1-26 September. Finally, the hourly mean distribution, obtained as difference BPOL (TUC-TEO) on the interval 7-9 September emphasizes an anomalous signal with five hours before the onset of the Mw8.1 earthquake.

摘要

在过去十年中,与罗马尼亚弗勒恰地震活动相关的实时地面地磁观测,以及与一些地震(2011年3月11日日本东北Mw9.0地震和2015年9月16日智利科金博大Mw8.3地震)相关的补充研究,扩展了我们对震前异常现象与地震成核最后阶段之间关系的认识。为了识别Mw8.1地震发生前可能的超低频(ULF)地磁信号,我们追溯分析了2017年8月1日至9月16日期间在墨西哥特洛约坎(TEO)和美国图森(TUC)地磁观测站收集的数据,并以后者作为参考。利用超低频范围(0.001 - 0.083赫兹)的快速傅里叶变换(FFT)带通滤波,获得了两个观测站的极化参数BPOL(地磁极化参数)和标准差的日均值分布。此外,我们研究了与Mw8.1地震相关的震前信号的奇异性,并应用基于标准化随机变量方程的统计分析;结果以9月1日至26日区间的BPOL*时间序列呈现。最后,9月7日至9日区间以BPOL(TUC - TEO)差值获得的每小时均值分布,突出了Mw8.1地震发生前五个小时的一个异常信号。

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