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  1. 防災科研関係論文

Postseismic displacements following the 2007 Noto peninsula earthquake detected by dense GPS observation

https://nied-repo.bosai.go.jp/records/5014
https://nied-repo.bosai.go.jp/records/5014
5b655dab-490f-4d69-8397-7eeb33f55fd5
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Postseismic displacements following the 2007 Noto peninsula earthquake detected by dense GPS observation
言語
言語 eng
著者 Manabu Hashimoto

× Manabu Hashimoto

en Manabu Hashimoto

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Hiroaki Takahashi

× Hiroaki Takahashi

en Hiroaki Takahashi

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Ryosuke Doke

× Ryosuke Doke

en Ryosuke Doke

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Minoru Kasahara

× Minoru Kasahara

en Minoru Kasahara

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Akira Takeuchi

× Akira Takeuchi

en Akira Takeuchi

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Kenusuke Onoue

× Kenusuke Onoue

en Kenusuke Onoue

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Yoshinobu Hoso

× Yoshinobu Hoso

en Yoshinobu Hoso

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Yo Fukushima

× Yo Fukushima

en Yo Fukushima

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Kajuro Nakamura

× Kajuro Nakamura

en Kajuro Nakamura

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Fumio Ohya

× Fumio Ohya

en Fumio Ohya

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Ryo Honda

× Ryo Honda

en Ryo Honda

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Masayoshi Ichiyanagi

× Masayoshi Ichiyanagi

en Masayoshi Ichiyanagi

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Teruhiro Yamaguchi

× Teruhiro Yamaguchi

en Teruhiro Yamaguchi

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Takahiro Maeda

× Takahiro Maeda

en Takahiro Maeda

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Yoshihiro Hiramatsu

× Yoshihiro Hiramatsu

en Yoshihiro Hiramatsu

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抄録
内容記述タイプ Other
内容記述 We have been conducting dense GPS observation in and around the epicentral region of the 2007 Noto peninsula earthquake since March 25, 2007, in order to detect postseismic displacements. Continuous observation has been underway at 12 sites to fill the gap of GEONET. Preliminary analysis of data up to early May shows that initial postseismic, displacement rapidly decayed within 20 days after the occurrence of the mainshock. Horizontal displacements do not exceed 20 mm even at sites above the aftershock zone for this period. We also found a maximum uplift of about 20 mm there. Inversion of postseismic displacements with the variable slip model suggests a nearly right-lateral afterslip of less than 5 cm on the shallow portion of the source fault. Fitting a theoretical function to a time series of coordinate changes also suggests that the observed postseismic displacements might have been generated by afterslip.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 60, 号 2, p. 139-144
出版者
言語 en
出版者 SPRINGER
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/BF03352775
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