ログイン
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

  1. 防災科研関係論文

Concentration of structural damage along surface fault ruptures during the 2016 Kumamoto earthquake

https://nied-repo.bosai.go.jp/records/7618
https://nied-repo.bosai.go.jp/records/7618
3b932dab-0c5b-47fa-a8c7-a079da3056b4
Item type researchmap(1)
公開日 2026-10-05
タイトル
言語 en
タイトル Concentration of structural damage along surface fault ruptures during the 2016 Kumamoto earthquake
言語
言語 eng
著者 Yasuhiro Suzuki

× Yasuhiro Suzuki

en Yasuhiro Suzuki

Search repository
Mitsuhisa Watanabe

× Mitsuhisa Watanabe

en Mitsuhisa Watanabe

Search repository
Takashi Nakata

× Takashi Nakata

en Takashi Nakata

Search repository
Kei Tanaka

× Kei Tanaka

en Kei Tanaka

Search repository
Hiroyuki Fujiwara

× Hiroyuki Fujiwara

en Hiroyuki Fujiwara

Search repository
Naokazu Monma

× Naokazu Monma

en Naokazu Monma

Search repository
Hiromitsu Nakamura

× Hiromitsu Nakamura

en Hiromitsu Nakamura

Search repository
Shohei Naito

× Shohei Naito

en Shohei Naito

Search repository
Asako Iwaki

× Asako Iwaki

en Asako Iwaki

Search repository
Shigeki Senna

× Shigeki Senna

en Shigeki Senna

Search repository
抄録
内容記述タイプ Other
内容記述 Building damage hazard due to earthquakes is a serious issue; however, quantitative analyses on the distribution of damages along surface fault ruptures are quite limited. Herein, we examine the relationship between the rate of structural damage and its distance from the surface fault during the 2016 Kumamoto earthquake. The earthquake caused severe damage to buildings along narrow zones adjacent to the 30-km-long surface fault. More than 90% of buildings that collapsed or suffered severe damage were located within 100 m of the fault, and the rate of collapse increased with the decrease in distance from the surface fault within the urbanized area of Mashiki Town. Such unique geographic distribution of structural damage cannot be fully explained by the influence of ground conditions or the general assumption that strong motions are not generated by surface faults, but rather by seismic source faults located at depths of more than a few kilometers. It may suggest the possibility of strong ground motion which was generated from a particularly shallow part of the seismic fault, which has been neglected in the current strong ground motion predictions. However, it is true that there were some areas close to the surface fault where no building damage occurred. The reasons for this are an important issue that needs to be investigated further.
言語 en
書誌情報 en : Journal of Disaster Science and Management

巻 2, 号 1, 発行日 2026-07-03
出版者
言語 en
出版者 Springer Science and Business Media LLC
ISSN
収録物識別子タイプ EISSN
収録物識別子 3005-1746
DOI
関連識別子 10.1007/s44367-026-00039-1
戻る
0
views
See details
Views

Versions

Ver.1 2026-09-28 01:51:04.288647
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR 2.0
  • OAI-PMH JPCOAR 1.0
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings