ŒfÚŽGŽi˜ajF | “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W |
VolF | 11Šª |
”NF |
2002”N
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•ÅF |
583-588•Å
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’˜ŽÒi˜ajF |
ù’J@ “wCXì@M”VC‘O“c@‹X_
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ƒ^ƒCƒgƒ‹i˜ajF |
1993”N‹ú˜H‰«’nk‚É‚æ‚é‹k“®‹L˜^FkŒ¹‹y‚Ñ“`”dŒo˜H“Á«‚Ì•]‰¿
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´˜^i˜ajF |
-
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ƒL[ƒ[ƒhi˜ajF |
ƒXƒ‰ƒu“à’nkC1993 ”N‹ú˜H‰«’nkCƒAƒXƒyƒŠƒeƒBƒ‚ƒfƒ‹C‰ž—Í~‰º—ÊC“`”dŒo˜H“Á«
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ŒfÚŽGŽi‰pjF |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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’˜ŽÒi‰pjF |
Tsutomu Sasatani, Nobuyuki Morikawa, Takahiro Maeda
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ƒ^ƒCƒgƒ‹i‰pjF |
STRONG MOTION RECORDS FROM THE 1993 KUSHIRO-OKI EARTHQUAKE: EVALUATION OF THE SOURCE AND PATH EFFECTS
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´˜^i‰pjF |
We have made a detailed analysis of strong motion records from the 1993 Kushiro-oki, intra-slab earthquake (Mw=7.6). First we evaluate an S-wave source spectrum of this event based on strong motion records at the fore-arc side of the volcanic front. The spectrum in the high-frequency range has extremely large amplitudes. Next we construct the source model using the empirical Green's function method. The source has three asperities with very high stress drops. Our estimates and previous studies show that the outer and inner fault parameters of this event have mutual relations proposed by Dan et al. (2002). Finally we investigate effects of the anomalous upper mantle structure on strong ground motions. The strong motion records at the back-arc side of the volcanic front show strong attenuation of short-period seismic waves.
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ƒL[ƒ[ƒhi‰pjF |
intra-slab earthquake, 1993 Kushiro-oki eathquake, asperity model, stress drop, path effect
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‹LŽ–‹æ•ªF |
-
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‹æ•ªF |
ˆÏˆõ‰ï˜_•¶W |