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  1. 防災科研関係論文

Ground Motions in the Fukushima Hamadori, Japan, Normal-Faulting Earthquake

https://nied-repo.bosai.go.jp/records/5335
https://nied-repo.bosai.go.jp/records/5335
d853a76a-6519-4aac-8522-2aecc8d6e36f
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Ground Motions in the Fukushima Hamadori, Japan, Normal-Faulting Earthquake
言語
言語 eng
著者 John G. Anderson

× John G. Anderson

en John G. Anderson

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Hiroshi Kawase

× Hiroshi Kawase

en Hiroshi Kawase

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Glenn P. Biasi

× Glenn P. Biasi

en Glenn P. Biasi

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James N. Brune

× James N. Brune

en James N. Brune

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Shin Aoi

× Shin Aoi

en Shin Aoi

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抄録
内容記述タイプ Other
内容記述 A crustal normal-faulting earthquake (M-JMA 7.0; M-w 6.7) occurred in eastern Tohoku, Japan, on 11 April 2011. K-NET and KiK-net stations recorded 82 records from within 100 km of fault rupture. These data and data from associated foreshocks and aftershocks will make a critical contribution to future improvements of ground-motion prediction for normal-faulting earthquakes.Peak ground accelerations (PGA) and peak ground velocities (PGV) are compared with four ground-motion prediction equations (GMPEs) that include the style of faulting as a predictor parameter. For distances under 100 km, and using a network average value of V-S30, the average ratio of PGA to the selected GMPEs (the event term) is high by factors of 2.3-3.7. Event terms for PGV are high by factors of 1.4-1.8. Adjusting PGA and PGV with customized site terms (Kawase and Matsuo, 2004a, b), the standard deviations of PGA and PGV residuals are reduced from 0.59 to 0.43, and from 0.53 to 0.35, respectively. The event terms decreased to relatively small factors of 1.1-1.8 for PGA and increased slightly to 1.5-2.0 for PGV. Thus, site terms are very important, but positive event terms remain. The remaining positive event terms are not explained by high stress drop, which was typical of crustal events of all mechanisms globally or in Japan. Two subparallel faults ruptured, but source inversions, which we reviewed, revealed that they ruptured sequentially, so simultaneous contributions from the two faults did not cause high motions. Although these observations may tend to suggest that ground motions in large normal-faulting events are larger than predicted by the tested models, we are not aware of any observations from this event that contradict the precarious rock evidence of Brune (2000) that ground shaking is low on the footwall near the rupture.
言語 en
書誌情報 en : BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA

巻 103, 号 3, p. 1935-1951
出版者
言語 en
出版者 SEISMOLOGICAL SOC AMER
ISSN
収録物識別子タイプ EISSN
収録物識別子 1943-3573
DOI
関連識別子 10.1785/0120120252
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