ŒfÚŽGŽi˜ajF | “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W |
VolF | 11Šª |
”NF |
2002”N
|
•ÅF |
119-124•Å
|
’˜ŽÒi˜ajF |
’r“c@FC‰Á“¡@Œ¤ˆêC•‘º@‰ë”V
|
ƒ^ƒCƒgƒ‹i˜ajF |
2001 ”NŒ|—\’nk‚Ì‚U“®”¬•ª‚Ì—ã‹N“Á«
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´˜^i˜ajF |
-
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ƒL[ƒ[ƒhi˜ajF |
Œ|—\’nkCƒXƒ‰ƒu“à’nkCkŒ¹ƒXƒyƒNƒgƒ‹C‚U“®”
|
ŒfÚŽGŽi‰pjF |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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’˜ŽÒi‰pjF |
Takashi Ikeda, Kenichi Kato, Masayuki Takemura
|
ƒ^ƒCƒgƒ‹i‰pjF |
GENERATION OF THE HIGH-FREQUENCY WAVE FOR THE 2001 GEIYO EARTHQUAKE
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´˜^i‰pjF |
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[ƒhi‰pjF |
Geiyo earthquake, Intra-plate earthquake, Source spectrum, High frequency
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‹LŽ–‹æ•ªF |
-
|
‹æ•ªF |
ˆÏˆõ‰ï˜_•¶W |