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  1. 防災科研関係論文

Cause of destructive strong ground motion within 1-2s in Mukawa town during the 2018 M-w 6.6 Hokkaido eastern Iburi earthquake

https://nied-repo.bosai.go.jp/records/5080
https://nied-repo.bosai.go.jp/records/5080
b8720d81-0c6b-483d-9b4d-a864c6ecb00a
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Cause of destructive strong ground motion within 1-2s in Mukawa town during the 2018 M-w 6.6 Hokkaido eastern Iburi earthquake
言語
言語 eng
著者 Nobuo Takai

× Nobuo Takai

en Nobuo Takai

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Michiko Shigefuji

× Michiko Shigefuji

en Michiko Shigefuji

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Jun Horita

× Jun Horita

en Jun Horita

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Shingo Nomoto

× Shingo Nomoto

en Shingo Nomoto

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Takahiro Maeda

× Takahiro Maeda

en Takahiro Maeda

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Masayoshi Ichiyanagi

× Masayoshi Ichiyanagi

en Masayoshi Ichiyanagi

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Hiroaki Takahashi

× Hiroaki Takahashi

en Hiroaki Takahashi

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Hiroaki Yamanaka

× Hiroaki Yamanaka

en Hiroaki Yamanaka

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Kosuke Chimoto

× Kosuke Chimoto

en Kosuke Chimoto

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Seiji Tsuno

× Seiji Tsuno

en Seiji Tsuno

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Masahiro Korenaga

× Masahiro Korenaga

en Masahiro Korenaga

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Nobuyuki Yamada

× Nobuyuki Yamada

en Nobuyuki Yamada

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抄録
内容記述タイプ Other
内容記述 We investigated the cause of destructive ground motion during the 2018 Hokkaido eastern Iburi earthquake. We conducted strong motion observations of aftershocks and microtremors and thesurface wave method in thedamaged areas of the town of Mukawa, Hokkaido prefecture, Japan. The ground accelerations were continuously recorded during a period of approximately 3months after the main shock on September 6, 2018. The heavily damaged buildings were mainly situated around the strong motion station (HKD126) in Mukawa town. Such concentration of damage can be explained by the strong power that was observed in the 1-2 s period of the response spectrum at this station. We estimated the S-wave velocity profiles of this station site and a temporary station site that was installed on a nearby hill. The estimated S-wave velocity, which was inverted from phase velocity structures with the microtremor array and the surface wave method observations explained the difference in the SH-wave amplification characteristics between the two sites. An analysis of HKD126 and the temporarily observed records clearly indicates the strong effects of thelocal geological conditions on the heavily damaged area of Mukawa. The strong ground motion power generated during the main shock in Mukawa for 1-2s periodwas mainly amplified by this shallow underground velocity structure.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 71
出版者
言語 en
出版者 SPRINGEROPEN
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-019-1044-4
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