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  1. 防災科研関係論文

The applicability of frictional reactivation theory to active faults in Japan based on slip tendency analysis

https://nied-repo.bosai.go.jp/records/4269
https://nied-repo.bosai.go.jp/records/4269
3a233d68-da17-4885-a8f9-6d7a8460cdf7
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル The applicability of frictional reactivation theory to active faults in Japan based on slip tendency analysis
言語
言語 eng
著者 Yohei Yukutake

× Yohei Yukutake

en Yohei Yukutake

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Tetsuya Takeda

× Tetsuya Takeda

en Tetsuya Takeda

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Akio Yoshida

× Akio Yoshida

en Akio Yoshida

Search repository
抄録
内容記述タイプ Other
内容記述 To investigate the applicability of frictional reactivation theory to active faults, we evaluated the slip tendency of active faults in Japan. Slip tendency is defined as the ratio of shear stress to the frictional resistance acting on a fault plane. To estimate the stress field near active faults, we determined focal mechanisms for numerous shallow earthquakes in the intraplate region of Japan, using data from dense seismic observation networks. The stress fields were estimated by applying the stress inversion method to the focal mechanisms. We found that most active faults are well oriented with respect to the stress field, having slip tendencies of >= 0.6, which indicates that fault reactivation theory is applicable to active faults, and that the present day tectonic stress field has contributed substantially to the development of active faults. Conversely, several steeply dipping active faults in northeast Japan, as well as the source faults of the 1995 Hyogoken-Nanbu earthquake, are mis-oriented, with slip tendencies of <0.6, which may indicate that highly pressurized fluids have contributed to earthquake triggering on these mis-oriented faults. We also discuss the applicability of slip tendency analysis to earthquake hazard assessment; i.e. estimating the probability of a future rupture on active faults. Our results indicate that slip tendency does not correlate with elapsed time since the most recent earthquake event. This observation shows that slip tendency may not be an efficient parameter with which to assess the risk of an earthquake occurring in the near future on a specific fault. (C) 2014 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : EARTH AND PLANETARY SCIENCE LETTERS

巻 411, p. 188-198, 発行日 2015-02
出版者
言語 en
出版者 ELSEVIER
ISSN
収録物識別子タイプ EISSN
収録物識別子 1385-013X
DOI
関連識別子 10.1016/j.epsl.2014.12.005
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