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  1. 防災科研関係論文

Stress fields and fault reactivation angles of the 2000 western Tottori aftershocks and the 2001 northern Hyogo swarm in southwest Japan

https://nied-repo.bosai.go.jp/records/4380
https://nied-repo.bosai.go.jp/records/4380
9f099331-664f-4db6-adfd-1fa8611bfc34
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Stress fields and fault reactivation angles of the 2000 western Tottori aftershocks and the 2001 northern Hyogo swarm in southwest Japan
言語
言語 eng
著者 A Kubo

× A Kubo

en A Kubo

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E Fukuyama

× E Fukuyama

en E Fukuyama

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抄録
内容記述タイプ Other
内容記述 We estimated the stress fields of the aftershocks of the 2000 western Tottori earthquake (M-w 6.6) and the northern Hyogo swarm (max M-w 5.2) by a stress tensor inversion of moment tensor solutions reported from the National Research Institute for Earth Science and Disaster Prevention (Japan). The maximum principal stress direction of the western Tottori sequence was estimated as N107degreesE with a strike-slip regime. In the northern Hyogo swarm, the orientations of the principal stress directions could not be well constrained by the observed data, but after examining the detailed characteristics of the solution, we obtained a most probable solution of N113degreesE for the sigma(1) direction. These solutions are consistent with the maximum horizontal directions roughly estimated from the strike directions of large earthquakes occurring geographically between these two seismic activities. We measured the angle between each fault-slip direction and maximum principal stress direction to investigate the frictional properties of earthquakes. The distribution of the angles was forward modeled to estimate the coefficient of friction and the stress ratio, assuming uniformly distributed fault orientations. For the western Tottori sequence, a homogeneous stress field with a coefficient of fiction less than 0.4 was estimated. A high stress level was also suggested because very little change occurred in the stress field during the mainshock. For the northern Hyogo sequence, the coefficient of friction was estimated to be between 0.5 and 1.0. (C) 2003 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : TECTONOPHYSICS

巻 378, 号 3-4, p. 223-239
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0040-1951
DOI
関連識別子 10.1016/j.tecto.2003.09.009
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