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  1. 防災科研関係論文

Ground motion and rupture process of the 2003 Tokachi-oki earthquake obtained from strong motion data of K-NET and KiK-net

https://nied-repo.bosai.go.jp/records/5974
https://nied-repo.bosai.go.jp/records/5974
3068e503-da8d-4bfc-9ef9-5ac112fcca9a
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Ground motion and rupture process of the 2003 Tokachi-oki earthquake obtained from strong motion data of K-NET and KiK-net
言語
言語 eng
著者 R Honda

× R Honda

en R Honda

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S Aoi

× S Aoi

en S Aoi

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N Morikawa

× N Morikawa

en N Morikawa

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H Sekiguchi

× H Sekiguchi

en H Sekiguchi

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T Kunugi

× T Kunugi

en T Kunugi

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H Fujiwara

× H Fujiwara

en H Fujiwara

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抄録
内容記述タイプ Other
内容記述 A great earthquake, named the 2003 Tokachi-oki earthquake, occurred in the southern Kuril subduction zone on 26th September 2003, 4:50 JST (41.7797degreesN, 144.0795degreesE, 42 km depth; Japan Meteorological Agency). Its ground motion was recoreded at 655 stations of the nationwide strong motion networks, K-NET and KiK-net. A maximum peak ground acceleration of 988 cm/s(2) (gal) was observed at station HKD100 and amplitudes greater than 200 cm/s(2) were observed over a wide area of eastern Hokkaido. We used a multi-line linear waveform inversion method to estimate the rupture process from the strong motion data of supplied by 15 stations. We assumed a fault plane model of 140 km x 160 km with strike and dip angles of our fault model are N246degreesE and 18degrees, respectively, placed on the estimated upper boundary of the subducting Pacific Plate. The estimated total slip distribution consisted of three major slip areas; (a) around the hypocenter, (b) the northwest part of the fault with the maximum slip of 5.9 m, and (c) the northeast edge of the fault plane. The major asperity (b) was composed of two large slip areas with different slip rate functions: the duration of moment release in the sourtheast part is longer than 15 see, but in contrast most of the seismic moment of the northwest part was released in a short period of less than 10 sec. Our estimation of the total seismic moment was 2.9 x 10(21) N(.)m which corresponded to Mw = 8.2.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 56, 号 3, p. 317-322, 発行日 2004
出版者
言語 en
出版者 SPRINGER HEIDELBERG
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 10.5636/eps.56.317
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