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地殻変動論ゼミ 5/16

地殻変動論ゼミ 5/16

セミナー等

SEMINARS

更新日:2019.04.10

Updated: 2019.04.10

  • 開催場所:防災研究所 本館2階E-232D
  • Place: 防災研究所 本館2階E-232D
  • 開催日時:2019年5月16日(木) 10時~
  • Date and Time: 2019年5月16日(木) 10時~

今週の地殻変動ゼミについて、日時と場所は以下のとおりです。

Here is information of the next seminar on crustal movements.

科目:地殻変動論ゼミナール(修士・博士)
日時:5月16日(木)10時00分~
場所:本館E232-D

西川友章学振特別研究員が下記の通り研究発表を行います。

Presenter: Tomoaki Nishikawa
Presentation title: Mapping the detailed distribution of slow earthquakes along the Japan Trench

Abstract: Investigating slow earthquake activity in subduction zones provides insights on the slip behavior of megathrusts, which is important to infer the rupture extent of future great earthquakes. Owing to a new ocean-bottom seismograph network along the Japan Trench, we mapped a detailed distribution of tectonic tremors, which coincided with very-low-frequency earthquakes and a slow slip event. Compiling these and other slow-earthquake-related observations, including repeating earthquakes and earthquake swarms, we show that the slow earthquake distribution is complementary to the Tohoku-Oki earthquake rupture. Our results suggest that the megathrust in the Japan Trench is divided into three along-strike segments characterised by different slip behavior, and that the rupture of the Tohoku-Oki earthquake, which nucleated in the central segment, was terminated by the two adjacent segments.


Date: 16 May, 2019 AM 10:00~
Place: E232D in Main Building

今週の地殻変動ゼミについて、日時と場所は以下のとおりです。

Here is information of the next seminar on crustal movements.

科目:地殻変動論ゼミナール(修士・博士)
日時:5月16日(木)10時00分~
場所:本館E232-D

西川友章学振特別研究員が下記の通り研究発表を行います。

Presenter: Tomoaki Nishikawa
Presentation title: Mapping the detailed distribution of slow earthquakes along the Japan Trench

Abstract: Investigating slow earthquake activity in subduction zones provides insights on the slip behavior of megathrusts, which is important to infer the rupture extent of future great earthquakes. Owing to a new ocean-bottom seismograph network along the Japan Trench, we mapped a detailed distribution of tectonic tremors, which coincided with very-low-frequency earthquakes and a slow slip event. Compiling these and other slow-earthquake-related observations, including repeating earthquakes and earthquake swarms, we show that the slow earthquake distribution is complementary to the Tohoku-Oki earthquake rupture. Our results suggest that the megathrust in the Japan Trench is divided into three along-strike segments characterised by different slip behavior, and that the rupture of the Tohoku-Oki earthquake, which nucleated in the central segment, was terminated by the two adjacent segments.


Date: 16 May, 2019 AM 10:00~
Place: E232D in Main Building

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© Research Center for Earthquake Hazards.

© Research Center for Earthquake Hazards.