@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W VolF 9-3Šª ”NF 1994”N •ÅF E.43-E.48•Å ’˜ŽÒi˜ajF - ƒ^ƒCƒgƒ‹i˜ajF - ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Kazuyoshi KUDO, Tsutomu SASATANI, Minoru SAKAUE, Seiji SAITO, Hideki NAGUMO, Masayoshi TAKAHASHI ƒ^ƒCƒgƒ‹i‰pjF EFFECTS OF SURFACE SOIL AND EARTHQUAKE SOURCE RADIATION ON THE GROUND MOTION OF 1.6G ACCELERATION, OBSERVED DURING THE AUGUST 8,1993, SOUTH-WEST OFF HOKKAIDO EARTHQUAKE JAPAN. ´˜^i‰pjF
We examined the reasons why the ground motion of 1.6g was observed at OTB from the largest aftershock of the 1993 SW-Off Hokkaido earthquake. The strongest effect was a large amplification due to shallow surface soils overlying hard rock. The amplification factor relative to rock motion was around 40 at a resonance frequency and roughly 10 for maximum amplitude in time domain. In addition, a source radiation effect was also significant. SV-waves from this event predominated in the direction to OTB. It is also plausible that the source directivity contributed to the large amplitude at OTB. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W