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Vol�F11Šª
”N�F 2002”N
•Å�F 119-124•Å
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ƒ^ƒCƒgƒ‹�i˜a�j�F 2001 ”NŒ|—\’n�k‚Ì�‚�U“®�”�¬•ª‚Ì—ã‹N“Á�«
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ƒL�[ƒ��[ƒh�i˜a�j�F Œ|—\’n�k�CƒXƒ‰ƒu“à’n�k�C�kŒ¹ƒXƒyƒNƒgƒ‹�C�‚�U“®�”
Œf�ÚŽGŽ��i‰p�j�F THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
’˜ŽÒ�i‰p�j�F Takashi Ikeda, Kenichi Kato, Masayuki Takemura
ƒ^ƒCƒgƒ‹�i‰p�j�F GENERATION OF THE HIGH-FREQUENCY WAVE FOR THE 2001 GEIYO EARTHQUAKE
�´˜^�i‰p�j�F The relation between peak ground acceleration Amax and peak ground velocity Vmax of the 2001 Geiyo earthquake is compared with other earthquakes. The ratio of Amax to Vmax, A/V of intra-plate earthquakes including the Geiyo earthquake is from 10 to 40 and is two times larger than that of inter-plate and crustal earthquakes. High-frequency components of seismic waves during main and after shocks of the Geiyo earthquake are examined from their source spectra. The stress drop ƒÐ that is calculated from the high-frequency flat level of acceleration source spectra is from 10 to 40MPa. This is almost equal to the level of ƒÐ of the other intra-plate earthquakes and is higher than that of inter-plate earthquakes.
ƒL�[ƒ��[ƒh�i‰p�j�F Geiyo earthquake, Intra-plate earthquake, Source spectrum, High frequency
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