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  1. 防災科研関係論文

CMT inversion for small-to-moderate earthquakes applying to dense short-period OBS array at off Ibaraki region

https://nied-repo.bosai.go.jp/records/3124
https://nied-repo.bosai.go.jp/records/3124
5071aa2e-1703-446b-bfed-f87f57449104
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル CMT inversion for small-to-moderate earthquakes applying to dense short-period OBS array at off Ibaraki region
著者 Lina Yamaya

× Lina Yamaya

en Lina Yamaya

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Kimihiro Mochizuki

× Kimihiro Mochizuki

en Kimihiro Mochizuki

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Takeshi Akuhara

× Takeshi Akuhara

en Takeshi Akuhara

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Shunsuke Takemura

× Shunsuke Takemura

en Shunsuke Takemura

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Masanao Shinohara

× Masanao Shinohara

en Masanao Shinohara

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Tomoaki Yamada

× Tomoaki Yamada

en Tomoaki Yamada

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抄録
内容記述タイプ Other
内容記述 We conducted centroid moment tensor (CMT) inversion for small-to-moderate aftershocks in the off Ibaraki region of the 2011 off the Pacific coast of Tohoku earthquake. In this study, we used high-frequency (0.4–1.0 Hz) seismograms from a dense array of short-period ocean bottom seismometers (OBSs) and a reliable three-dimensional (3-D) seismic velocity model. Higher frequency analysis and dense OBS arrays offer CMT solutions with high spatial resolutions. Since our OBS array observed aftershocks occurring immediately following the 2011 off the Pacific coast of Tohoku earthquake, we determined 536 CMT solutions for small-to-moderate aftershocks in the off Ibaraki region (JMA-scale magnitudes of 2.5–4.0). According to our CMT solutions, characteristics of the aftershock activities in the off Ibaraki region are classified into 5 groups: (1) thrust earthquakes, which are considered as interplate earthquakes, separated by the large slip area of the 2011 Ibaraki-oki earthquake (the largest M w 7.6 aftershock of the 2011 off the Pacific coast of Tohoku earthquake) and the tectonic tremors; (2) intraslab strike-slip earthquakes located at the north of the fault area of the 2011 Ibaraki-oki earthquake; (3) intraslab normal-fault earthquakes, which suggest a tensional stress field within the subducting Pacific Plate due to the plate bending by the overriding Philippine Sea Plate; (4) various earthquake focal mechanisms above a subducting seamount, which suggest the 3-D complex fractures; and (5) normal-fault earthquakes shallower than the interplate earthquakes, which were possibly caused by the heterogeneity of the subducting seamount. Graphical Abstract: [Figure not available: see fulltext.].
言語 en
書誌情報 en : Earth, Planets and Space

巻 74, 号 1, 発行日 2022-11-08
ISSN
収録物識別子タイプ EISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-022-01721-3
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