Slip distribution of the 1952 Tokachi-Oki earthquake (M8.1) along the Kuril Trench deduced from tsunami waveform inversion

Author:

Hirata Kenji1,Geist Eric1,Satake Kenji2,Tanioka Yuichiro3,Yamaki Shigeru4

Affiliation:

1. U.S. Geological Survey; Menlo Park California USA

2. Active Fault Research Center; National Institute of Advanced Industrial Science and Technology; Tsukuba Japan

3. Meteorological Research Institute; Tsukuba Japan

4. Seamus Ltd.; Niigata Japan

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference56 articles.

1. Reliability of a tsunami source model derived from fault parameters;Aida;J. Phys. Earth,1978

2. Tides in the English channel and southern North Sea. A frequency domain analysis using Model TEA-NL;Baptista;Adv. Water Resour.,1989

3. Linearized inversion for fault rupture behavior; application to the 1984 Morgan Hill, California, earthquake;Beroza;J. Geophys. Res.,1988

4. Rigidity variations with depth along interplate megathrust faults in subduction zones;Bilek;Science,1999

5. Report of the Tokachi-Oki earthquake of March 4, 1952;Central Meteorological Observatory;Q. J. Seismol,1953

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