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In contrast, along the northern and central Hikurangi margin, short-term and shallow (\u003c10 km) SSEs (2- to 3-week duration) occur at 1- to 2-year intervals. However, it is not clear what controls these differences in SSE behavior. In this study, we simulate SSEs along the entire Hikurangi subduction zone using a 3-D model of the plate boundary incorporating a rate-and-state friction law with a cutoff velocity to the evolution effect. Overall, our models are able to replicate the along-strike and depth-dependent variations in SSE behavior at the Hikurangi margin. Our models also show that the slip velocities of the deep, long-term SSEs increase when the slip velocities at the deeper extension of the seismogenic zone increase during the latter half of the interseismic period. By imposing static stress changes induced by the Kaikoura earthquake in the SSE regions, we also reproduce patterns of triggering of deep, long-term SSEs that followed the earthquake. 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Wallace", "creatorNameLang": "ja"}, {"creatorName": "Laura M. 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  1. 防災科研関係論文

Three‐Dimensional Modeling of Spontaneous and Triggered Slow‐Slip Events at the Hikurangi Subduction Zone, New Zealand

https://nied-repo.bosai.go.jp/records/4594
https://nied-repo.bosai.go.jp/records/4594
c9824d44-dff1-41d3-934e-eab8594dafd0
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Three‐Dimensional Modeling of Spontaneous and Triggered Slow‐Slip Events at the Hikurangi Subduction Zone, New Zealand
タイトル
言語 en
タイトル Three-Dimensional Modeling of Spontaneous and Triggered Slow-Slip Events at the Hikurangi Subduction Zone, New Zealand
言語
言語 eng
著者 Bunichiro Shibazaki

× Bunichiro Shibazaki

ja Bunichiro Shibazaki

en Bunichiro Shibazaki

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Laura M. Wallace

× Laura M. Wallace

ja Laura M. Wallace

en Laura M. Wallace

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Yoshihiro Kaneko

× Yoshihiro Kaneko

ja Yoshihiro Kaneko

en Yoshihiro Kaneko

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Ian Hamling

× Ian Hamling

ja Ian Hamling

en Ian Hamling

Search repository
Yoshihiro Ito

× Yoshihiro Ito

ja Yoshihiro Ito

en Yoshihiro Ito

Search repository
Takanori Matsuzawa

× Takanori Matsuzawa

ja Takanori Matsuzawa

en Takanori Matsuzawa

Search repository
抄録
内容記述タイプ Other
内容記述 At the southern Hikurangi margin, New Zealand, long-term (duration of >1 year), deep (>25 km) slow-slip events (SSEs) occur at intervals of approximately 5 years. In contrast, along the northern and central Hikurangi margin, short-term and shallow (<10 km) SSEs (2- to 3-week duration) occur at 1- to 2-year intervals. However, it is not clear what controls these differences in SSE behavior. In this study, we simulate SSEs along the entire Hikurangi subduction zone using a 3-D model of the plate boundary incorporating a rate-and-state friction law with a cutoff velocity to the evolution effect. Overall, our models are able to replicate the along-strike and depth-dependent variations in SSE behavior at the Hikurangi margin. Our models also show that the slip velocities of the deep, long-term SSEs increase when the slip velocities at the deeper extension of the seismogenic zone increase during the latter half of the interseismic period. By imposing static stress changes induced by the Kaikoura earthquake in the SSE regions, we also reproduce patterns of triggering of deep, long-term SSEs that followed the earthquake. Our results further suggest that the propensity for SSE triggering via static stress transfer depends on the amplitude of perturbation and the timing with respect to the SSE cycle. Overall, both spontaneous and triggered SSEs require larger values of effective stress for deep, long-term events (5 MPa) compared to the shallow, short-term events (1 MPa). Such low effective stresses can be explained by the existence of high pore fluid pressure in these SSE source regions.
言語 en
書誌情報 ja : Journal of Geophysical Research: Solid Earth
en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 124, 号 12, p. 13250-13268, 発行日 2019-12
出版者
言語 ja
出版者 American Geophysical Union ({AGU})
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-9356
DOI
関連識別子 10.1029/2019JB018190
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