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  1. 防災科研関係論文

Coseismic and postseismic deformation related to the 2007 Chuetsu-oki, Niigata Earthquake

https://nied-repo.bosai.go.jp/records/5027
https://nied-repo.bosai.go.jp/records/5027
9396c2f9-895b-4bb2-8417-e8317c62a981
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Coseismic and postseismic deformation related to the 2007 Chuetsu-oki, Niigata Earthquake
言語
言語 eng
著者 Yusaku Ohta

× Yusaku Ohta

en Yusaku Ohta

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Satoshi Miura

× Satoshi Miura

en Satoshi Miura

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Takeshi Iinuma

× Takeshi Iinuma

en Takeshi Iinuma

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Kenji Tachibana

× Kenji Tachibana

en Kenji Tachibana

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Takeshi Matsushima

× Takeshi Matsushima

en Takeshi Matsushima

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Hiroaki Takahashi

× Hiroaki Takahashi

en Hiroaki Takahashi

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Takeshi Sagiya

× Takeshi Sagiya

en Takeshi Sagiya

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Takeo Ito

× Takeo Ito

en Takeo Ito

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Shin'ichi Miyazaki

× Shin'ichi Miyazaki

en Shin'ichi Miyazaki

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Ryosuke Doke

× Ryosuke Doke

en Ryosuke Doke

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Akira Takeuchi

× Akira Takeuchi

en Akira Takeuchi

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Kayo Miyao

× Kayo Miyao

en Kayo Miyao

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Akihiko Hirao

× Akihiko Hirao

en Akihiko Hirao

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Takahiro Maeda

× Takahiro Maeda

en Takahiro Maeda

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Teruhiro Yamaguchi

× Teruhiro Yamaguchi

en Teruhiro Yamaguchi

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Masamitsu Takada

× Masamitsu Takada

en Masamitsu Takada

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Makiko Iwakuni

× Makiko Iwakuni

en Makiko Iwakuni

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Tadafumi Ochi

× Tadafumi Ochi

en Tadafumi Ochi

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Irwan Meilano

× Irwan Meilano

en Irwan Meilano

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Akira Hasegawa

× Akira Hasegawa

en Akira Hasegawa

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抄録
内容記述タイプ Other
内容記述 An intermediate-strength earthquake of magnitude M(j) 6.8 occurred on July 16, 2007, centered beneath the Japan Sea a few kilometers offshore of Niigata Prefecture in central Japan. We constructed a dense GPS network to investigate postseismic deformation after this event, choosing our GPS sites carefully so as to complement the nationwide GPS GEONET array. Coseismic displacements caused by the mainshock detected at some GEONET sites were used to estimate coseismic fault parameters. The results indicate that the geodetic data can be explained by a combination of two rectangular faults dipping northwest and southeast. Minor but definite postseismic deformation was detected largely in the southern part of the dense network. The time series of site coordinates can be characterized by a logarithmic decay function, and the estimated time constant seems to be almost similar in range to that of the 2004 Mid-Niigata Prefecture Earthquake. We also found a possible site instability at 960566 (Izurno-zaki, GEONET) caused by a small, local landslide associated with the mainshock and therefore concluded that the data obtained at this site should not be used for coseismic or postseismic analysis.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 60, 号 11, p. 1081-1086
出版者
言語 en
出版者 TERRA SCIENTIFIC PUBL CO
ISSN
収録物識別子タイプ ISSN
収録物識別子 1343-8832
DOI
関連識別子 10.1186/BF03353140
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