@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W VolF 9-1Šª ”NF 1994”N •ÅF 415-420•Å ’˜ŽÒi˜ajF ì£ ”Ž ƒ^ƒCƒgƒ‹i˜ajF ‹CÛ’¡‚W‚VŒ^‹­kŒv‹L˜^‚É‚æ‚é–kŠC“¹Žü•Ó‚Ì’nk‚ÌkŒ¹“Á«‚Æ“¹“à‹CÛ‘ä‚̃TƒCƒg“Á« ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Hiroshi KAWASE ƒ^ƒCƒgƒ‹i‰pjF SOURCE CHARACTERISTICS OF EARTHQUAKS AROUND HOKKAIDO AND SITE RESPONSES OF JMA STATIONS OBTAINED FROM JMA87-TYPE STRONG-MOTION RECORDS ´˜^i‰pjF
Strong motion records of 11 earthquakes, including the Kushiro-Oki earthquake of 1993, observed at 10 JMA stations in Hokkaido were analysed. If local site amplification for each station may not be so large the averaged spectra corrected for attenuation will be flat for wide frequency range. First path effects are corrected by appropriate Q to have averaged hypocentral spectra. Then a local site factor at each site is calculated as a ratio between the observed spectra and the averaged one. It is found that the Kushiro station has strong local effect whose peak frequency and amplification ratio are 3.6Hz and 10, respectively. During the Kushiro-Oki earthquake peak frequency decreases to 2.8Hz, which may suggest the presence of non-linear effect. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W