Source Process of Megathrust Earthquakes along the Sagami Trough Deduced from Seismic Intensity Data

Author:

KANDA Katsuhisa1,TAKEMURA Masayuki1

Affiliation:

1. Kobori Research Complex, Kajima Corporation

Publisher

Japan Association for Earthquake Engineering

Reference5 articles.

1. 7) Ohno, S., T. Ohta, T. Ikeura and M. Takemura: Revision of attenuation formula considering the effect of fault size to evaluate strong motion spectra in near field, Tectonophysics, Vol.218, 1993, pp.69-81.

2. 10) Ishida, M.: Geometry and relative motion of the Philippine Sea Plate and Pacific Plate beneath he Kanto-Tokai district, Japan, J. Geophys. Res., Vol.97, No.B1, 1992, pp.489-513.

3. 11) Sato, H., N. Hirata, K. Koketsu, D. Okaya, S. Abe, R. Kobayashi, M. Matsubara, T. Iwasaki, T. Ito, T. Ikawa, T. Kawanaka, K. Kasahara and S. Harder: Earthquake source fault beneath Tokyo, Science, Vol.309, No.5733, 2005, pp.337-520.

4. 15) Wald, J.W. and P.G. Somerville: Variable-slip rupture model of the Great 1923 Kanto, Japan earthquake: Geodetic and body-waveform analysis, Bull. Seism. Soc. Am., Vol.85, No.1, 1995, pp.159-177.

5. 16) Nakahara, H., T. Nishimura, H. Sato and M. Ohtake: Seismogram envelope inversion for the spatial distribution of high-frequency energy radiation from the earthquake fault: Application to the 1994 far east off Sanriku earthquake, Japan, J. Geophys. Res., 103, B1, 1998, pp.855-867.

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