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  1. 防災科研関係論文

Aftershock observation of the 2003 Tokachi-oki earthquake by using dense ocean bottom seismometer network

https://nied-repo.bosai.go.jp/records/5021
https://nied-repo.bosai.go.jp/records/5021
43618f9f-a208-4721-b1f2-1137ebcb1c22
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 ja
タイトル Aftershock observation of the 2003 Tokachi-oki earthquake by using dense ocean bottom seismometer network
タイトル
言語 en
タイトル Aftershock observation of the 2003 Tokachi-oki earthquake by using dense ocean bottom seismometer network
著者 Masanao Shinohara

× Masanao Shinohara

ja Masanao Shinohara

en Masanao Shinohara

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Tomoaki Yamada

× Tomoaki Yamada

ja Tomoaki Yamada

en Tomoaki Yamada

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Toshihiko Kanazawa

× Toshihiko Kanazawa

ja Toshihiko Kanazawa

en Toshihiko Kanazawa

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Naoshi Hirata

× Naoshi Hirata

ja Naoshi Hirata

en Naoshi Hirata

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Yoshiyuki Kaneda

× Yoshiyuki Kaneda

ja Yoshiyuki Kaneda

en Yoshiyuki Kaneda

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Tetsuo Takanami

× Tetsuo Takanami

ja Tetsuo Takanami

en Tetsuo Takanami

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Hitoshi Mikada

× Hitoshi Mikada

ja Hitoshi Mikada

en Hitoshi Mikada

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Kiyoshi Suyehiro

× Kiyoshi Suyehiro

ja Kiyoshi Suyehiro

en Kiyoshi Suyehiro

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Shin'ichi Sakai

× Shin'ichi Sakai

ja Shin'ichi Sakai

en Shin'ichi Sakai

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Tomoki Watanabe

× Tomoki Watanabe

ja Tomoki Watanabe

en Tomoki Watanabe

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Kenji Uehira

× Kenji Uehira

ja Kenji Uehira

en Kenji Uehira

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Yoshio Murai

× Yoshio Murai

ja Yoshio Murai

en Yoshio Murai

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Narumi Takahashi

× Narumi Takahashi

ja Narumi Takahashi

en Narumi Takahashi

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Minoru Nishino

× Minoru Nishino

ja Minoru Nishino

en Minoru Nishino

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Kimihiro Mochizuki

× Kimihiro Mochizuki

ja Kimihiro Mochizuki

en Kimihiro Mochizuki

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Takeshi Sato

× Takeshi Sato

ja Takeshi Sato

en Takeshi Sato

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Ei'ichiro Araki

× Ei'ichiro Araki

ja Ei'ichiro Araki

en Ei'ichiro Araki

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Ryota Hino

× Ryota Hino

ja Ryota Hino

en Ryota Hino

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Kouichi Uhira

× Kouichi Uhira

ja Kouichi Uhira

en Kouichi Uhira

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Hajime Shiobara

× Hajime Shiobara

ja Hajime Shiobara

en Hajime Shiobara

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Hiroshi Shimizu

× Hiroshi Shimizu

ja Hiroshi Shimizu

en Hiroshi Shimizu

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抄録
内容記述タイプ Other
内容記述 The Tokachi-Oki earthquake occurred on September 26, 2003. Precise aftershock distribution is important to understand the mechanism of this earthquake generation. To study the aftershock activity, we deployed forty-seven ocean bottom seismometers (OBSs) and two ocean bottom pressure meters (OBPs) at thirty-eight sites in the source region. We started the OBS observation four days after the mainshock for an observation period of approximately two months. In the middle of the observation period, nine OBSs near the epicenter of the mainshock were recovered to clarify the depth distribution of aftershocks near the mainshock. From the data overall OBS, seventy-four aftershocks were located with high spatial resolution. Most of the aftershocks were located in a depth range of 15-20 km and occurred within the subducting oceanic crust, the 5.5-km/s layer of the landward plate and the plate boundary. No aftershocks were found in the mantle of the subducting plate. The low seismic activity beneath the trench area where the water depth is greater than about 2000 m suggests a weak coupling between the two plates. The depth of the mainshock is inferred to be 15-20 km from the aftershock distribution. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences.
言語 ja
抄録
内容記述タイプ Other
内容記述 The Tokachi-Oki earthquake occurred on September 26, 2003. Precise aftershock distribution is important to understand the mechanism of this earthquake generation. To study the aftershock activity, we deployed forty-seven ocean bottom seismometers (OBSs) and two ocean bottom pressure meters (OBPs) at thirty-eight sites in the source region. We started the OBS observation four days after the mainshock for an observation period of approximately two months. In the middle of the observation period, nine OBSs near the epicenter of the mainshock were recovered to clarify the depth distribution of aftershocks near the mainshock. From the data overall OBS, seventy-four aftershocks were located with high spatial resolution. Most of the aftershocks were located in a depth range of 15-20 km and occurred within the subducting oceanic crust, the 5.5-km/s layer of the landward plate and the plate boundary. No aftershocks were found in the mantle of the subducting plate. The low seismic activity beneath the trench area where the water depth is greater than about 2000 m suggests a weak coupling between the two plates. The depth of the mainshock is inferred to be 15-20 km from the aftershock distribution. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences.
言語 en
書誌情報 ja : Earth, Planets and Space
en : Earth, Planets and Space

巻 56, 号 3, p. 295-300
出版者
言語 en
出版者 Springer Science and Business Media LLC
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/BF03353054
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