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  1. 防災科研関係論文

High-V-P/V-S zone accompanying non-volcanic tremors and slow-slip events beneath southwestern Japan

https://nied-repo.bosai.go.jp/records/4384
https://nied-repo.bosai.go.jp/records/4384
c78d600c-c379-45e4-93fd-cdeaf863a0d2
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル High-V-P/V-S zone accompanying non-volcanic tremors and slow-slip events beneath southwestern Japan
言語
言語 eng
著者 Makoto Matsubara

× Makoto Matsubara

en Makoto Matsubara

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Kazushige Obara

× Kazushige Obara

en Kazushige Obara

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Keiji Kasahara

× Keiji Kasahara

en Keiji Kasahara

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抄録
内容記述タイプ Other
内容記述 In southwestern Japan, the Philippine Sea plate subducts beneath the Eurasian plate. Non-volcanic tremors and slow slow-slip events are observed beneath southwestern Japan. Seismic tomography based on the data obtained from the dense seismic network revealed the velocity structure in and around the subducting Philippine Sea plate. The oceanic crust of the Philippine Sea plate subducting from the Suruga and Nankai troughs can be imaged clearly beneath the Tokai region and the Kii peninsula. Non-volcanic tremors and short-term slow-slip events may occur in the high-V-P/V-S zones owing to the fluid dehydrated from the subducting plate where the oceanic crust of the Philippine Sea plate encounters the serpentinized wedge mantle of the Eurasian plate. These tremors and short-term slow-slip events occur in the high-V-P/V-S zone at depths of 30-40 km beneath the Tokai region, the landward edge of the high-V-P/V-S zone beneath the Kii peninsula and eastern Shikoku region, and the seaward edge of the high-V-P/V-S zone beneath the western Shikoku region. Long-term slow-slip events were observed beneath the Tokai region and the Bungo channel and both these events are located on the seaward side of a high-V-P/V-S zone. These long-term slow-slip events are considered to be caused at the plate boundary between the oceanic crust of the Philippine Sea plate and the lower crust of the Eurasian plate by the high pore-fluid pressure caused by the fluid dehydrated from the subducting plate. The existence of the high-V-P/V-S lower crust of the Eurasian plate may control the occurrence of the long-term slow-slip events. (c) 2008 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : TECTONOPHYSICS

巻 472, 号 1-4, p. 6-17
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
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.2008.06.013
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