更新日:2019.04.10
Updated: 2019.04.10
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
© Research Center for Earthquake Hazards.
© Research Center for Earthquake Hazards.