@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€u‰‰W VolF 7Šª ”NF 1986”N •ÅF 115-120•Å ’˜ŽÒi˜ajF - ƒ^ƒCƒgƒ‹i˜ajF - ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Shigeru NODA, Hiroshi OISHI, Eiji UEMATSU ƒ^ƒCƒgƒ‹i‰pjF ESTIMATION OF NEAR-SOURCE GROUND MOTIONS OF THE 1980 IZU-HANTO-TOHO-OKI EARTHQUAKE BY DWFE METHOD ´˜^i‰pjF
In this study, the discrete wavenumber/finite element (DWFE) method (Olson, 1982) and the fault dislocation theory were applied to the case of the Izu-Hanto-Toho-Oki earthquake (M=6.7) of 1980. Ground motions were computed at the site of Kawana near the source region. The displacement seismograms synthesized from the theoretical method were compared with the actual strong-motion records. We were able to reproduce the recorded waveforms, particularly of body waves and the first portion of surface waves, by the theoretical synthesis method with a realistic crustal structure. The best agreement between the observed and synthesized waveforms was obtained for relatively long-period components with periods of 0.5-6 sec. The acceleration response spectra calculated gave a good estimate of those observed over the period range from 0.5 to about 10 sec . ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W