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Seismological aspects of the Japan Sea earthquake of 1983
Author(s) -
Hirasawa Tomowo
Publication year - 1983
Publication title -
disasters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.744
H-Index - 70
eISSN - 1467-7717
pISSN - 0361-3666
DOI - 10.1111/j.1467-7717.1983.tb00831.x
Subject(s) - seismology , geology , aftershock , focal mechanism , tectonics , intraplate earthquake , trench , foreshock , tsunami earthquake , seismic gap , interplate earthquake , fault plane , fault (geology) , magnitude (astronomy) , chemistry , organic chemistry , layer (electronics) , physics , astronomy
The Japan Sea earthquake of 1983 took place at the eastern margin of the Japan Sea, which is a marginal sea situated west of the island are of Japan and the Japan trench in the Pacific Ocean. Its magnitude of 7.7 is the largest among earthquakes which have been known to occur in the seismic belt along the Japan Sea coast of Northeast Honshu, Japan. Since the seismic activity in the belt is not so high, the earthquake is especially important in the geophysical interpretation of tectonic process in the region. The aftershock distribution and the focal mechanism reveals that the earthquake is a thrust fault on a plane dipping eastwards by about 30°. The waveform analysis shows that the earthquake can be regarded as a double shock to a first approximation. Interestingly, there was a 10‐second intermission between the two events. These are preliminary results, and more detailed studies are under development.