PROPAGATION CHARACTERISTIC OF THE BASIN EDGE INDUCED WAVE AT THE WESTERN EDGE OF THE KANTO BASIN OBSERVED FROM THE CONTINUOUS RECORD OF MeSO-net
Author:
Affiliation:
1. Faculty of Engineering and Design, Kagawa Univ.
Publisher
Architectural Institute of Japan
Subject
Building and Construction,Architecture
Link
https://www.jstage.jst.go.jp/article/aijs/87/793/87_251/_pdf
Reference19 articles.
1. 1) Kawase, H. : Review : Amplification of Seismic Waves by Sedimentary Layers and Its Simulation, Zisin Second Series, Vol. 46, No.2, pp. 171-190. 1993 (in Japanese) 川瀬博 : 表層地質による地震波の増幅とそのシミュレーション, 地震 第 2輯, Vol. 46, No. 2, pp. 171-190, 1993
2. 2) Kawase, H. : The cause of the damage belt in Kobe : “The basin-edge effect,” constructive interference of the direct S-wave with the basin-induced diffracted/Rayleigh waves, Seism. Res. Lett., Vol. 67, No. 5, pp.25-34, 1996
3. 3) Kawase, H. and K. Aki : A study on the response of a soft basin for incident S, P, and Rayleigh waves with special reference to the long duration observed in Mexico City, Bull. Seism. Soc. Am., Vol. 79, pp. 1361-1382, 1989
4. 4) National Research Institute for Earth Science and Disaster Resilience : NIED K-NET, KiK-net, National Research Institute for Earth Science and Disaster Resilience, doi:10.17598/NIED.0004, 2019
5. 5) Miyake, H., K. Koketsu : Long-period ground motions from a large offshore earthquake: The case of the 2004 off the Kii peninsula earthquake, Japan, Earth Planets Space, Vol. 57, pp. 203-207, 2005
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