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Dynamic rupture propagation during the 1891 Nobi, central Japan, earthquake: A possible extension to the branched faults
https://nied-repo.bosai.go.jp/records/5324
https://nied-repo.bosai.go.jp/records/532448e4c1cd-d0e6-4b58-a9be-1d0115e27c12
Item type | researchmap(1) | |||||||||
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公開日 | 2023-03-30 | |||||||||
タイトル | ||||||||||
言語 | en | |||||||||
タイトル | Dynamic rupture propagation during the 1891 Nobi, central Japan, earthquake: A possible extension to the branched faults | |||||||||
言語 | ||||||||||
言語 | eng | |||||||||
著者 |
Eiichi Fukuyama
× Eiichi Fukuyama
× Takeshi Mikumo
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抄録 | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | The dynamic rupture process of the 1891 Nobi, Japan, earthquake was closely reinvestigated by using a boundary integral equation method based on currently available observations. We discussed mainly a possibility of the rupture propagation on branched faults, including a buried fault called the Gifu-Ichinomiya line. Several numerical simulations were made incorporating the information on the fault geometry based on the active fault traces on the ground surface and the maximum principal strain direction observed by the triangular surveys for the past 100 years. The results suggest that the rupture should propagate along the buried fault during the Nobi earthquake if a weak geological discontinuity exists along the Gifu-Ichinomiya line and is connected to the Neodani fault, which is one of the major surface faults appearing during the Nobi earthquake. | |||||||||
言語 | en | |||||||||
書誌情報 |
en : BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA 巻 96, 号 4, p. 1257-1266 |
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出版者 | ||||||||||
言語 | en | |||||||||
出版者 | SEISMOLOGICAL SOC AMER | |||||||||
ISSN | ||||||||||
収録物識別子タイプ | ISSN | |||||||||
収録物識別子 | 0037-1106 | |||||||||
DOI | ||||||||||
関連識別子 | 10.1785/0120050151 |