Art

J-GLOBAL ID：201402288376080612   Reference number：14A0969033

What Caused the 2011 Tohoku-Oki Earthquake?: Effects of Dynamic Weakening

何が2011年東北沖地震を引き起こしたのか?:動的弱化の効果

Author (2)： SHIBAZAKI Bunichiro (Building Res. Inst., Ibaraki, JPN) ,  NODA Hiroyuki (Japan Agency for Marine-Earth Sci. and Technol., Kanagawa, JPN)
Material： Journal of Disaster Research  (J Disaster Res)
Volume： 9  Issue： 3  Page： 252-263  Publication year： Jun. 01, 2014 
JST Material Number： F1399A  ISSN： 1881-2473  Document type： Article
Article type： 文献レビュー  Country of issue： Japan (JPN)  Language： ENGLISH (EN)

Thesaurus term： *large earthquake ,  law ,  constitutive equation ,  Japan Trench ,  subduction zone ,  model ,  thermal effect ,  *The 2011 off the Pacific coast of Tohoku Earthquake ,  *subduction-zone earthquake ,  slip weakening rule
Semi thesaurus term： frictional constitutive law

JST classification (1)： Physics of the earth's interior in general  (DC03010P)

Reference (44)：

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• S. Ide, A. Baltay, and G. C. Beroza, “Shallow dynamic overshoot and energetic deep rupture in the 2011 M_w9.0 Tohoku-Oki earthquake,” Science, Vol.332, pp. 1426-1429, doi:10.1126/science.1207020, 2011.
• Y. Ito, T. Tsuji, Y. Osada, M. Kido, D. Inazu, Y. Hayashi, H. Tsushima, R. Hino, and H. Fujimoto, “Frontal wedge deformation near the source region of the 2011 Tohoku-Oki earthquake,” Geophys. Res. Lett., Vol.38, L00G05, doi:10.1029/2011GL048355, 2011.
• T. Lay, C. J. Ammon, H. Kanamori, L. Xue, and M. J. Kim, “Possible large near trench slip during the 2011 M_w9.0 the Pacific coast of Tohoku Earthquake,” Earth Planets Space, Vol.63, pp. 687-692, doi:10.5047/eps.2011.05.033, 2011.
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Terms in the title (1)： 東北沖地震