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  1. 防災科研関係論文

Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes

https://nied-repo.bosai.go.jp/records/4011
https://nied-repo.bosai.go.jp/records/4011
7b98b9f7-37ee-4294-ad81-48d12b6619d8
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes
言語
言語 eng
著者 Youichi Asano

× Youichi Asano

en Youichi Asano

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Kazushige Obara

× Kazushige Obara

en Kazushige Obara

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Takanori Matsuzawa

× Takanori Matsuzawa

en Takanori Matsuzawa

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Hitoshi Hirose

× Hitoshi Hirose

en Hitoshi Hirose

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Yoshihiro Ito

× Yoshihiro Ito

en Yoshihiro Ito

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抄録
内容記述タイプ Other
内容記述 We investigated the spatiotemporal evolution of a shallow very low frequency earthquake (sVLFE) swarm linked to the 2009/2010 long-term slow slip event (SSE) in the Bungo channel, southwestern Japan. Broadband seismograms were analyzed using a cross-correlation technique to detect sVLFEs having similar waveforms to template sVLFEs, and their relative locations were estimated. The sVLFEs exhibit clear migration over a distance of 150km along the Nankai trough, similar to nonvolcanic tremors and deep very low frequency earthquakes (dVLFEs) accompanied by short-term SSEs on the downward extension of the seismogenic zone. This similarity between sVLFEs and dVLFEs suggests that SSEs occur in both deeper and shallower extensions of the seismogenic zone. The analyzed sVLFEs were likely caused by a shallow SSE that occurred from January to March 2010 following the initiation and acceleration of the long-term SSE. This temporal evolution may be caused by stress interaction between the shallow SSE and the long-term SSE.
言語 en
書誌情報 en : GEOPHYSICAL RESEARCH LETTERS

巻 42, 号 2, p. 331-338
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 1944-8007
DOI
関連識別子 10.1002/2014GL062165
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