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  1. 防災科研関係論文

Spatiotemporal complexity of 2-D rupture nucleation process observed by direct monitoring during large-scale biaxial rock friction experiments

https://nied-repo.bosai.go.jp/records/2827
https://nied-repo.bosai.go.jp/records/2827
1b954c85-d5a5-4b39-adf8-4eae478ffa76
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Spatiotemporal complexity of 2-D rupture nucleation process observed by direct monitoring during large-scale biaxial rock friction experiments
言語
言語 eng
著者 Eiichi Fukuyama

× Eiichi Fukuyama

en Eiichi Fukuyama

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Kotoyo Tsuchida

× Kotoyo Tsuchida

en Kotoyo Tsuchida

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Hironori Kawakata

× Hironori Kawakata

en Hironori Kawakata

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Futoshi Yamashita

× Futoshi Yamashita

en Futoshi Yamashita

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Kazuo Mizoguchi

× Kazuo Mizoguchi

en Kazuo Mizoguchi

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Shiqing Xu

× Shiqing Xu

en Shiqing Xu

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抄録
内容記述タイプ Other
内容記述 We were able to successfully capture rupture nucleation processes on a 2-D fault surface during large-scale biaxial friction experiments using metagabbro rock specimens. Several rupture nucleation patterns have been detected by a strain gauge array embedded inside the rock specimens as well as by that installed along the edge walls of the fault. In most cases, the unstable rupture started just after the rupture front touched both ends of the rock specimen (i.e., when rupture front extended to the entire width of the fault). In some cases, rupture initiated at multiple locations and the rupture fronts coalesced to generate unstable ruptures, which could only be detected from the observation inside the rock specimen. Therefore, we need to carefully examine the 2-D nucleation process of the rupture especially when analyzing the data measured only outside the rock specimen. At least the measurements should be done at both sides of the fault to identify the asymmetric rupture propagation on the fault surface, although this is not perfect yet. In the present experiment, we observed three typical types of the 2-D rupture propagation patterns, two of which were initiated at a single location either close to the fault edge or inside the fault. This initiation could be accelerated by the free surface effect at the fault edge. The third one was initiated at multiple locations and had a rupture coalescence at the middle of the fault. These geometrically complicated rupture initiation patterns are important for understanding the earthquake nucleation process in nature.
言語 en
書誌情報 en : Tectonophysics

巻 733, p. 182-192, 発行日 2018-05-09
出版者
言語 en
出版者 Elsevier B.V.
ISSN
収録物識別子タイプ ISSN
収録物識別子 0040-1951
DOI
関連識別子 10.1016/j.tecto.2017.12.023
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