日本地球惑星科学連合2016年大会

講演情報

インターナショナルセッション(口頭発表)

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT18] Stress geomechanics: observations, modelings and implications

2016年5月22日(日) 09:00 〜 10:30 302 (3F)

コンビーナ:*呉 泓昱(海洋研究開発機構)、Chan Chung-Han(南洋理工大学)、斎藤 実篤(国立研究開発法人海洋研究開発機構)、真田 佳典((独)海洋研究開発機構)、宮川 歩夢(独立行政法人 産業技術総合研究所 地質情報研究部門)、山田 泰広(海洋研究開発機構 海洋掘削科学研究開発センター)、座長:Chung-Han Chan(Earth Observatory of Singapore, Nanyang Technological University)

10:15 〜 10:30

[STT18-06] Stress changes and the displacement of an out-of-sequence thrust in an accretionary wedge

*宮川 歩夢1山田 泰広2大坪 誠1 (1.国立研究開発法人 産業技術総合研究所、2.国立研究開発法人 海洋研究開発機構)

キーワード:numerical simulation, stress change, out-of-sequence thrust

The stress state in an accretionary wedge is one of the most important topics in subduction zone, hence fault activities are related to the surrounding stress regime in an accretionary wedge. Many study try to represent the stress state related to the fault activity in the accretionary wedge (e.g. Hashimoto et al. 2014; Yamada & Shibanuma 2015). However, the measurement of stress in an accretionary wedge remains challenging, especially that of dynamic stress changes due to fault activity. Here we propose the stress changes associate with the displacement of an Out-of-sequence thrusts (OOSTs) by using numerical simulation. In our numerical simulation, the likelihood of fault slip around the OOST is higher before a large slip event than those after the event, suggesting that the OOST was activated during a period of high likelihood of fault slip and that the likelihood of fault slip drops after slip upon the OOST. The stress changes associated with fault activity in the numerical simulation are consistent with those reported for natural OOSTs (Otsubo et al. under review).