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  1. 防災科研関係論文

Structure of the tsunamigenic plate boundary and low?frequency earthquakes in the southern Ryukyu Trench

https://nied-repo.bosai.go.jp/records/4618
https://nied-repo.bosai.go.jp/records/4618
64a4438e-a0eb-46a9-ba41-60dad2b94b4f
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Structure of the tsunamigenic plate boundary and low?frequency earthquakes in the southern Ryukyu Trench
タイトル
言語 en
タイトル Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
言語
言語 eng
著者 Ryuta Arai

× Ryuta Arai

ja Ryuta Arai

en Ryuta Arai

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Tsutomu Takahashi

× Tsutomu Takahashi

ja Tsutomu Takahashi

en Tsutomu Takahashi

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Shuichi Kodaira

× Shuichi Kodaira

ja Shuichi Kodaira

en Shuichi Kodaira

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Yuka Kaiho

× Yuka Kaiho

ja Yuka Kaiho

en Yuka Kaiho

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Ayako Nakanishi

× Ayako Nakanishi

ja Ayako Nakanishi

en Ayako Nakanishi

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Gou Fujie

× Gou Fujie

ja Gou Fujie

en Gou Fujie

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Yasuyuki Nakamura

× Yasuyuki Nakamura

ja Yasuyuki Nakamura

en Yasuyuki Nakamura

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Yojiro Yamamoto

× Yojiro Yamamoto

ja Yojiro Yamamoto

en Yojiro Yamamoto

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Yasushi Ishihara

× Yasushi Ishihara

ja Yasushi Ishihara

en Yasushi Ishihara

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Seiichi Miura

× Seiichi Miura

ja Seiichi Miura

en Seiichi Miura

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Yoshiyuki Kaneda

× Yoshiyuki Kaneda

ja Yoshiyuki Kaneda

en Yoshiyuki Kaneda

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抄録
内容記述タイプ Other
内容記述 It has been recognized that even weakly coupled subduction zones may cause large interplate earthquakes leading to destructive tsunamis. The Ryukyu Trench is one of the best fields to study this phenomenon, since various slow earthquakes and tsunamis have occurred; yet the fault structure and seismic activity there are poorly constrained. Here we present seismological evidence from marine observation for megathrust faults and low-frequency earthquakes (LFEs). On the basis of passive observation we find LFEs occur at 15-18 km depths along the plate interface and their distribution seems to bridge the gap between the shallow tsunamigenic zone and the deep slow slip region. This suggests that the southern Ryukyu Trench is dominated by slow earthquakes at any depths and lacks a typical locked zone. The plate interface is overlaid by a low-velocity wedge and is accompanied by polarity reversals of seismic reflections, indicating fluids exist at various depths along the plate interface.
言語 en
書誌情報 ja : Nature Communications
en : NATURE COMMUNICATIONS

巻 7, 号 12255, 発行日 2016-07
出版者
言語 en
出版者 NATURE PUBLISHING GROUP
ISSN
収録物識別子タイプ ISSN
収録物識別子 2041-1723
DOI
関連識別子 10.1038/ncomms12255
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