JpGU-AGU Joint Meeting 2017

講演情報

[EJ] 口頭発表

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT32] [EJ] Recent earthquakes and deep structure of the Earth in and around Tibetan Plateau

2017年5月24日(水) 10:45 〜 12:15 103 (国際会議場 1F)

コンビーナ:白 玲(ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences)、Mori James(京都大学防災研究所地震防災研究部門)、佐藤 比呂志(東京大学地震研究所地震予知研究センター)、石川 有三(国立研究開発法人 産業技術研究所 活断層・火山研究部門)、座長:白 玲(ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences)、座長:Mori James(京都大学防災研究所)、座長:佐藤 比呂志(東京大学地震研究所)、座長:石川 有三(国立研究開発法人 産業技術研究所 活断層・火山研究部門)

11:30 〜 11:45

[SIT32-04] The very low frequency earthquakes (VLFEs) relation with the 2008’s great Wenchuan earthquake

*jin deng

キーワード:very low-frequency earthquakes(VLF), Low-frequency events, the 2008’Wenchuan 8.0 earthquake

This study reports discovery of very low frequency earthquakes (VLFEs) that occurred 4 h before the 2008 Ml=8.0 Wenchuan earthquake. The VLF events swarm is of 35 events, recorded by China seismic monitoring network between 10:00 to 12:00 on 12 May 2008. The VLFEs are characterized by waveform durations of 1000-2000 s, magnitudes of Mw2-4 and focal depths 25-40 km deeper than those of natural earthquakes in the same regions. The VLFs last arrived phase is reflected wave and clearly to be identified in VLFs waveform, as fig.1. The VLF waveforms is from more than one events with its Pg arrival times.
The VLFEs swarm can be one of important precursor evidence before the large earthquake.