ŒfÚŽGŽi˜ajF | “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W |
VolF | 11Šª |
”NF |
2002”N
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•ÅF |
579-582•Å
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’˜ŽÒi˜ajF |
’r“c@—²–¾CŠ˜]@ŽGCŽO—Ö@Ž C“ü‘q@FŽŸ˜Y
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ƒ^ƒCƒgƒ‹i˜ajF |
ƒnƒCƒuƒŠƒbƒh–@‚É‚æ‚é2000 ”N’¹ŽæŒ§¼•”’nk‚Ì‹k“®ƒVƒ~ƒ…ƒŒ[ƒVƒ‡ƒ“
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´˜^i˜ajF |
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ƒL[ƒ[ƒhi˜ajF |
ƒnƒCƒuƒŠƒbƒh–@CLŽüŠú‘шæC2000 ”N’¹ŽæŒ§¼•”’nkC‹k“®CÅ“KkŒ¹ƒ‚ƒfƒ‹
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ŒfÚŽGŽi‰pjF |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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’˜ŽÒi‰pjF |
Takaaki Ikeda, Katsuhiro Kamae, Shigeru Miwa, Kojiro Irikura
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ƒ^ƒCƒgƒ‹i‰pjF |
STRONG GROUND MOTION SIMULATION OF THE 2000 TOTTORI-KEN SEIBU EARTHQUAKE USING THE HYBRID TECHNIQUE
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´˜^i‰pjF |
We simulated broadband strong ground motions during the 2000 Tottori-Ken Seibu earthquake using the hybrid technique. The long period motions and short period motion are simulated using the 1-D wave-number integration method and the stochastic Green's function method [Kamae et al. (1991)], respectively. Broadband strong ground motion was made by adding long period motion and short period motion in time domain. Source model used here has been estimated by the forward modeling using the empirical Green's function method [Ikeda et al. (2001)]. Broadband strong ground motions have been simulated in the K-Net and KiK-Net observation sites surrounding the source area. The effectiveness of the hybrid technique and the validity of the source model have been shown by the comparison between the synthetics and the observed ones.
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ƒL[ƒ[ƒhi‰pjF |
Hybrid technique, Broadband, 2000 Tottori-Ken Seibu earthquake, Strong ground motion, Best source model
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‹LŽ–‹æ•ªF |
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‹æ•ªF |
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