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  1. 防災科研関係論文

Dynamic rupture activation of backthrust fault branching

https://nied-repo.bosai.go.jp/records/4395
https://nied-repo.bosai.go.jp/records/4395
00b84c12-e0b2-439b-8bc5-4cf1633163c9
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Dynamic rupture activation of backthrust fault branching
言語
言語 eng
著者 Shiqing Xu

× Shiqing Xu

en Shiqing Xu

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Eiichi Fukuyama

× Eiichi Fukuyama

en Eiichi Fukuyama

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Yehuda Ben-Zion

× Yehuda Ben-Zion

en Yehuda Ben-Zion

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Jean-Paul Ampuero

× Jean-Paul Ampuero

en Jean-Paul Ampuero

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抄録
内容記述タイプ Other
内容記述 We perform dynamic rupture simulations to investigate the possible reactivation of backthrust branches triggered by ruptures along a main thrust fault. Simulations with slip-weakening fault friction and uniform initial stress show that fast propagation speed or long propagation distance of the main rupture promotes reactivation of backthrust over a range of branch angles. The latter condition may occur separately from the former if rupture speed is limited by an increasing slip-weakening distance towards the junction direction. The results suggest a trade-off between the amplitude and duration of the dynamic stress near the main rupture front for backthrust reactivation. Termination of the main rupture by a barrier can provide enhanced loading amplitude and duration along a backthrust rooted near the barrier, facilitating its reactivation especially with a high frictional resistance. The free surface and depth-dependent initial stress can have several additional effects. The sign of the triggered motion along the backthrust can be reversed from thrust to normal if a deeply nucleated main rupture breaks the free surface, while it is preserved as thrust if the main rupture is terminated by a barrier at depth. The numerical results are discussed in relation to several recent megathrust earthquakes in Sumatra, Chile, and Japan, and related topics such as branch feedbacks to the main fault. The dynamic view on backthrust fault branching provided by the study fills a gap not covered by quasi-static models or observations. A specific examined case of antithetic fault branching may be useful for indicating a barrier-like behavior along the main fault. (C) 2015 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : TECTONOPHYSICS

巻 644, p. 161-183
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ EISSN
収録物識別子 1879-3266
DOI
関連識別子 10.1016/j.tecto.2015.01.011
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