Generating Factor of Strong Ground Motions for a period of 2 to 3 seconds Observed in the Western Part of Tokyo Bay, during the 2011 off the Pacific Coast of Tohoku Earthquake
Author:
Affiliation:
1. Railway Technical Research Institute
2. Tokyo Institute of Technology
3. East Japan Railway Company
4. Earthquake Research Institute, University of Tokyo
Publisher
Japan Association for Earthquake Engineering
Link
https://www.jstage.jst.go.jp/article/jaee/16/4/16_4_35/_pdf
Reference12 articles.
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2. 15) Koketsu, K. and Kikuchi, M. : Propagation of Seismic Ground Motion in the Kanto Basin, Japan, Science, 288(5469), 2000, pp.1237-1239.
3. 16) Miyake, H. and Koketsu, K. : Long-Period Ground Motions from a Large Offshore Earthquake:The Case of the 2004 off the Kii Peninsula Earthquake, Japan, EPS, 57, 2005, pp.203-207.
4. 19) Ishihara, K., Muroi, T. and Towhata, I. : In-Situ Pore Water Pressures and Ground Motions during the 1987 Chiba-Toho-Oki Earthquake, Soils and Foundations, Vol.29, No.4, 1989, pp.75-90.
5. 21) Sakai, S. and Hirata, N. : Distribution of the Metropolitan Seismic Observation Network, Bull. Earthq. Res. Inst. Univ. Tokyo, 84, 2009, pp.57-69.
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1. Azimuthal dependence on amplifications for long-period ground motions propagating in the Kanto Basin, Japan;Journal of Seismology;2022-03-15
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