首页> 外文期刊>Physica, A. Statistical mechanics and its applications >Analysis of the ultra-low frequency magnetic field fluctuations prior to the 2016 Kumamoto (Japan) earthquakes in terms of the method of critical fluctuations
【24h】

Analysis of the ultra-low frequency magnetic field fluctuations prior to the 2016 Kumamoto (Japan) earthquakes in terms of the method of critical fluctuations

机译:在临界波动方法中,2016年熊本(日本)地震前超低频率磁场波动分析

获取原文
获取原文并翻译 | 示例
           

摘要

The method of critical fluctuations (MCF) is a time series analysis method which provides a way of both identifying the critical state and the departure from it. Its application to the ground-based ultra-low frequency (ULF) magnetic field fluctuations observed prior to the very strong earthquakes (EQs) of magnitudes M-W = 6.2, M-W = 6.0 and M-W = 7.0 which sequentially took place within a two days period (April 14-15, 2016) in Southwest Japan under the city of Kumamoto reveals when the underlying process reached critical state, as well as when it departed from critical state. Specifically, critical dynamics was identified in the raw total geomagnetic field intensity (F) ULF recordings of the Kanoya (Japan) station similar to 4 d before the M-W = 6.2 and similar to 5 d before the M-W = 7.0 event. Moreover, the progressive development of the symmetry breaking phenomenon, which signifies departure from critical state, was identified in later recordings. Specifically the phenomenon evolved from a few hours before the M-W = 6.0 event until a few hours after the occurrence of the specific EQ which was a few hours before the M-W = 7.0 event. The detected combination of phenomena, i.e., the detection of critical state followed by the detection of the departure from the critical state by means of symmetry breaking, indicates that the main event was the third and strongest EQ while the two preceding EQs were strong foreshocks. (C) 2018 Elsevier B.V. All rights reserved.
机译:临界波动(MCF)的方法是一个时间序列分析方法,其提供了一种方式来识别临界状态和离境。它在基于地面的超低频率(ULF)磁场波动之前观察到的大地震(EQS)的大= 6.2,MW = 6.0和MW = 7.0在两天内顺序发生( 2016年4月14日至15日)在日本西南市下的熊本市下揭示了潜在的过程达到了临界状态,以及当它离开临界状态时。具体而言,在M-W = 6.2之前的4D和M-W = 7.0之前的活动之前,Kanoya(日本)站的原始总地质磁场强度(F)ULF记录中识别了临界动态。此外,在后面的录音中确定了对称性破坏现象的逐步发展,这意味着偏离临界状态。具体地,在M-W = 6.0之前几小时开始的现象在特定EQ发生之后几小时发展,在M-W = 7.0事件前几个小时。检测到的现象组合,即临界状态的检测,然后通过对称性断开检测偏离临界状态的偏离,表明主事件是第三和最强的EQ,而前面的两个EQS是强大的预科。 (c)2018年elestvier b.v.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号