2007年6月12日希腊Lesvos地震前的长记忆和分形轨迹:基于DFA和时变谱分形的研究

D. Nikolopoulos, H. Panayiotis, P. Ermioni, C. Demetrios, N. Constantinos
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引用次数: 8

摘要

本文展示了在距离震中仅44公里的遥测地面站(39.23°N/26.27°E)记录的ML=6.1浅层地震(2017年6月12日,12:28:38 GMT, 38.84°N/26.36°E, 12公里深,37.5公里SSE,希腊莱斯沃斯岛Mytilene镇)之前收集的一个月kHz-MHz电磁干扰的长期和混乱趋势的证据。所有分析的地震(4.0≤ML< 6.1)在时间和空间上都形成了紧密的群体,这对调查具有重要意义。分析是通过详细的时间演变滑动窗口双斜率DFA和每个窗口4096个样本的幂律分析来实现的,允许隐藏的,潜在的前兆,震前趋势出现。经典的双指数DFA结果支持ML=6.1地震前10-12天可能的震前活动方面,对于3-10 kHz天线(包括EW-NS方向)和41-46 MHz天线,同时呈现由两个DFA指数数据计算的参数突然增加。幂律分形分析数据的时间演化表明在事件发生之前的12-13次活动,然而,仅针对3 kHz天线。在各分析段计算的Hurst指数表明了主要震前活动的持续性以及持续性-反持续性变化。对另外两次ML=5.0和ML=4.6地震的潜在震前活动进行了调查和讨论。讨论了已报道的时间序列的前兆活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-Memory and Fractal Traces in KHz-MHz Electromagnetic Time Series Prior to the ML=6.1, 12/6/2007 Lesvos, Greece Earthquake: Investigation through DFA and Time-Evolving Spectral Fractals
This paper presents evidence of long-lasting and chaotic trends in one-month kHz-MHz electromagnetic disturbances collected prior to a ML=6.1 shallow earthquake (June 12, 2017, 12:28:38 GMT, 38.84° N/26.36° E, 12 km deep, 37.5 km SSE of Mytilene town, Lesvos island, Greece) recorded by a telemetric ground station (39.23° N/26.27° E) located only 44 km away from the earthquake's epicenter. All analyzed earthquake occurrences (4.0 ≤ ML< 6.1) formed tight groups in both time and space which is significant for the investigation. The analysis is implemented via detailed timeevolving sliding-window two-slope DFA and power-law analysis of 4096 samples per window allowing hidden, potentially precursory, pre-earthquake trends to emerge. The classical two-exponent DFA results support the aspect of possible pre-earthquake activity 10-12 days prior to the ML=6.1 earthquake, for the 3-10 kHz antennas (both EW-NS orientations) and the 41-46 MHz ones, by simultaneously presenting a sudden increase of a parameter calculated from the two DFA exponent data. The time evolution of the power-law fractal-analysis data indicates activity 12-13 prior to the event, however, only for the 3 kHz antennas. Hurst exponents calculated in various analysis segments indicate persistency during the main pre-earthquake activity as well as persistency-anti-persistency changes. Potential pre-seismic activity prior to two other earthquakes of ML=5.0 and ML=4.6 is investigated and discussed. The precursory activity of reported time-series is discussed.
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