首页> 外文期刊>Advances in Geosciences >Characterization of the seismic dynamical state through joint analysis of earthquakes and seismic noise: the example of Ischia Volcanic Island (Italy)
【24h】

Characterization of the seismic dynamical state through joint analysis of earthquakes and seismic noise: the example of Ischia Volcanic Island (Italy)

机译:通过地震和地震噪声联合分析来表征地震动力学状态:伊斯基亚火山岛的举例(意大利)

获取原文
       

摘要

This work is devoted to the study of both earthquakes and background seismicnoise at Ischia Island (Italy) recorded pre and post the M _(d) ?4.0 earthquakeoccurred on 21?August?2017 (18:57 UTC). We compare and characterize noiseand earthquakes in terms of Independent Component Analysis, energy andpolarization properties. The earthquakes' waveforms and the background noiseare decomposed into a few independent components with two main commonsignals peaked around 1–2 and 3–4 Hz , respectively. A slight increase ofthe energy of the background seismic noise is observed comparing samplesrecorded in 2016 and 2017, whereas no variations are detected in 2017 preand post the main earthquake. The polarization analysis, performed in thefrequency bands individuated by Independent Component Analysis and appliedto the background seismic noise, indicates a shallow propagation and theazimuthal pattern is mainly controlled by the local structural features.These results suggest that noise and earthquakes are ascribable to a commonphenomenon of fluid-solid interaction in the hydrothermal system of IschiaIsland.
机译:这项工作致力于在Ischia岛(意大利)录制的地震和背景地震发作的研究录制了预先并发布了 m _(d)?4.0大地震诊断21岁?八月?2017(18:57 UTC)。我们在独立分量分析,能量和偏振性质方面进行比较和表征噪音地震。地震的波形和背景Noiseare分解成几个独立的组件,分别达到1-2和3-4 Hz的两个主要偶数。观察到2016年和2017年的样品,观察到背景地震噪声的能量略微增加,而2017年在2017年普通地震中没有检测到任何变化。在独立分量分析和应用于背景地震噪声的自杀带中进行的偏振分析表明浅传播和神化模式主要由局部结构特征控制。这些结果表明噪声和地震归类为液体的常见的液体 - 伊斯基亚岛水热系统中的 - 溶解相互作用。

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