@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W VolF 9-3Šª ”NF 1994”N •ÅF E.67-E.72•Å ’˜ŽÒi˜ajF - ƒ^ƒCƒgƒ‹i˜ajF - ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Hao Xian-Sheng, Kenji HAGIO, Toshiro MAEDA, Hiroshi HIBINO, Reiko YAMANAKA ƒ^ƒCƒgƒ‹i‰pjF A SITE RESPONSE ESTIMATION IN KUSHIRO CITY BASED ON A COMPARISON BETWEEN MICROTREMORS AND WEAK-MOTION ´˜^i‰pjF
After the 1993 Kushiro-Oki Earthquake(M=7.8), microtremor measurements were conducted in Kushiro city, Hokkaido, Japan. During the measurement, a weak ground motion caused by an earthquake happened to be recorded. In this paper, Fourier spectral ratio has been used to compare the characteristics of the microtremors to those of the weak motion induced by the earthquake. Fourier spectral characteristics of the microtremors, recorded in a six day period, are very similar with those of the weak-motion, indicating that the behavior is independent of the excitation characteristics, that is rather strongly related to the local geological structure. More specifically, spectral ratio characteristics of S waves and surface waves were found very similar, while those of P waves were different between the microtremors and the weak-motion. This might suggest that, in the range of periods between 0.1 to 10 seconds, microtremors are mainly composed of shear waves and surface waves. Finally, distribution of the predominant periods in Kushiro city was estimated by the spectral ratio method. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W