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  1. 防災科研関係論文

Reliable fault modeling of an Mw 7.1 earthquake in Hyuganada Sea on 8 August 2024 by offshore tsunami data from new seafloor network N‐net and onshore GNSS data

https://nied-repo.bosai.go.jp/records/7098
https://nied-repo.bosai.go.jp/records/7098
e0957109-7f12-4782-ab87-4518a727bbd7
Item type researchmap(1)
公開日 2025-04-28
タイトル
言語 ja
タイトル Reliable fault modeling of an Mw 7.1 earthquake in Hyuganada Sea on 8 August 2024 by offshore tsunami data from new seafloor network N‐net and onshore GNSS data
タイトル
言語 en
タイトル Reliable fault modeling of an Mw 7.1 earthquake in Hyuganada Sea on 8 August 2024 by offshore tsunami data from new seafloor network N‐net and onshore GNSS data
言語
言語 eng
著者 Tatsuya Kubota

× Tatsuya Kubota

ja Tatsuya Kubota

en Tatsuya Kubota

Search repository
Hisahiko Kubo

× Hisahiko Kubo

ja Hisahiko Kubo

en Hisahiko Kubo

Search repository
Tatsuhiko Saito

× Tatsuhiko Saito

ja Tatsuhiko Saito

en Tatsuhiko Saito

Search repository
抄録
内容記述タイプ Other
内容記述 We investigated tsunamis of an Mw 7.1 earthquake in the Hyuganada Sea in 2024, observed by a new dense and wide seafloor observation network, N‐net, installed in the western Nankai Trough. A joint inversion of the offshore tsunami and onshore GNSS data revealed a maximum slip of 2.4?m with a significant slip near the centroid from the teleseismic analysis. The joint inversion provided reliable constraints for both up‐dip and down‐dip extents of the fault, while the inversions using either data set showed limitations in the fault constraint. Comparisons with past earthquakes indicate the 2024 earthquake ruptured part of the asperity of the 1961 earthquake but not those of the 1996 earthquakes. Our fault modeling jointly using offshore and onshore data suggests the interplate seismic coupling ratio in this region is?<0.4, which was much smaller than those in the anticipated megathrust earthquake source region in the Nankai Trough.
言語 ja
抄録
内容記述タイプ Other
内容記述 We investigated tsunamis of an Mw 7.1 earthquake in the Hyuganada Sea in 2024, observed by a new dense and wide seafloor observation network, N‐net, installed in the western Nankai Trough. A joint inversion of the offshore tsunami and onshore GNSS data revealed a maximum slip of 2.4?m with a significant slip near the centroid from the teleseismic analysis. The joint inversion provided reliable constraints for both up‐dip and down‐dip extents of the fault, while the inversions using either data set showed limitations in the fault constraint. Comparisons with past earthquakes indicate the 2024 earthquake ruptured part of the asperity of the 1961 earthquake but not those of the 1996 earthquakes. Our fault modeling jointly using offshore and onshore data suggests the interplate seismic coupling ratio in this region is?<0.4, which was much smaller than those in the anticipated megathrust earthquake source region in the Nankai Trough.
言語 en
書誌情報 ja : Geophysical Research Letters
en : Geophysical Research Letters

巻 52, p. e2025115391, 発行日 2025-04-23
出版者
言語 ja
出版者 American Geophysical Union
出版者
言語 en
出版者 American 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 10.1029/2025GL115391
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