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On Possible Electromagnetic Precursors to a Significant Earthquake (Mw = 6.3) Occurred in Lesvos (Greece) on 12 June 2017

机译:在2017年6月12日在Lesvos(希腊)发生的可能电磁前体(MW = 6.3)发生在Lesvos(Greece)

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摘要

This paper reports an attempt to use ultra-low-frequency (ULF) magnetic field data from a space weather monitoring magnetometer array in the study of earthquake (EQ) precursors in Greece. The data from four magnetometer stations of the HellENIc GeoMagnetic Array (ENIGMA) have been analyzed in the search for possible precursors to a strong EQ that occurred south of Lesvos Island on 12 June 2017, with magnitude Mw = 6.3 and focal depth = 12 km. The analysis includes conventional statistical methods, as well as criticality analysis, using two independent methods, the natural time (NT) method and the method of critical fluctuations (MCF). In terms of conventional statistical methods, it is found that the most convincing ULF precursor was observed in the data of ULF (20–30 mHz) depression (depression of the horizontal component of the magnetic field), which is indicative of lower ionospheric perturbation just 1 day before the EQ. Additionally, there are indications of a precursor in the direct ULF emission from the lithosphere 4 days to 1 day before the EQ. Further study in terms of NT analysis identifies criticality characteristics from 8 to 2 days before the EQ both for lithospheric ULF emission and ULF depression, while MCF reveals indications of criticality in all recorded magnetic field components, extending from 10 to 3 days before the EQ. Beyond the recordings of the geomagnetic stations of ENIGMA, the recordings of the fracto-electromagnetic emission stations of the HELlenic Seismo-ElectroMagnetics Network (ELSEM-Net) in Greece have been analyzed. The MHz recordings at the station that is located on Lesvos Island presented criticality characteristics (by means of both NT analysis and MCF) 11 days before the EQ, while a few days later (7–6 days before the EQ), the kHz recordings of the same station presented tricritical behavior. It is noted that the magnetosphere was quiet for a period of two weeks before the EQ and including its occurrence.
机译:本文报告了尝试在希腊地震(EQ)前体的研究中使用来自空间天气监测磁力计阵列中的超低频率(ULF)磁场数据。在2017年6月12日在Lesvos岛南部出现的强大EQ的搜索中,已经分析了来自希腊地磁阵列(ENIGMA)的四个磁仪站的数据,幅度MW = 6.3和焦深= 12公里。分析包括常规统计方法,以及使用两个独立方法,自然时间(NT)方法和临界波动方法(MCF)的常规分析。就常规统计方法而言,发现在ULF(20-30MHz)凹陷(磁场水平部件的凹陷)数据中观察到最令人信服的ULF前体,这表明刚刚较低的电离层扰动平等前一天。另外,在岩石圈的直接ULF排放中存在前体的指示4天至12天前1天。在NT分析方面的进一步研究将EQ均为岩石层ULF排放和ULF抑郁症的8至2天鉴定了临界特征,而MCF揭示了所有记录的磁场组分中临界性的指示,从EQ之前的10至3天延伸。除了谜的地磁站的录音之外,已经分析了希腊希腊地震电磁网络(ELSEM-Net)的逆转电磁站的录音。位于Lesvos Island的车站的MHz录音呈现临界特征(通过NT分析和MCF)在EQ之前11天,而几天后(EQ前7-6天),KHz录音同一站呈现了三重批判行为。值得注意的是,磁圈在方程前两周的时间安静,包括其发生。

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