Heterogeneous structure across the source regions of the 1968 Tokachi-Oki and the 1994 Sanriku-Haruka-Oki earthquakes at the Japan Trench revealed by an ocean bottom seismic survey

Author:

Hayakawa Tadaaki,Kasahara Junzo,Hino Ryota,Sato Toshinori,Shinohara Masanao,Kamimura Aya,Nishino Minoru,Sato Takeshi,Kanazawa Toshihiko

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference38 articles.

1. Crustal structure in a profile off the Pacific coast of northeastern Japan by the refraction method with ocean bottom seismometer;Asano;J. Phys. Earth,1981

2. Fujie, G., 1999. A new travel time inversion using refracted and reflected arrivals and its application to the estimation of the plate boundary structure off Sanriku, Japan. Dr. Sci. Thesis, University of Tokyo, Tokyo (in Japanese).

3. Traveltime and raypath computation: a new method in a heterogeneous medium;Fujie;Butsuri-Tansa,2000

4. Inhomogeneous crustal structure and seismic activity at the plate subduction zone, off Sanriku region;Fujie;J. Geogr.,2000

5. Gebrande, H., 1982. Elastic wave velocities and constants of elasticity of rocks at room temperature and pressures up to 1 GPa. In: Angenheister, G. (Ed.), Physical Properties of Rocks, Vol. 1. Springer, Berlin, pp. 35–99.

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