| Œf�ÚŽGŽ��i˜a�j�F | “ú–{’n�k�HŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶�W |
| Vol�F | 11Šª |
| ”N�F |
2002”N
|
| •Å�F |
119-124•Å
|
| ’˜ŽÒ�i˜a�j�F |
’r“c�@�F�C‰Á“¡�@Œ¤ˆê�C•�‘º�@‰ë”V
|
| ƒ^ƒCƒgƒ‹�i˜a�j�F |
2001 ”NŒ|—\’n�k‚Ì�‚�U“®�”�¬•ª‚Ì—ã‹N“Á�«
|
| �´˜^�i˜a�j�F |
-
|
| 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
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| ’˜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
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| �´˜^�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.
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| ƒL�[ƒ��[ƒh�i‰p�j�F |
Geiyo earthquake, Intra-plate earthquake, Source spectrum, High frequency
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| ‹LŽ–‹æ•ª�F |
-
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| ‹æ•ª�F |
ˆÏˆõ‰ï˜_•¶�W |