�@ Œf�ÚŽGŽ��i˜a�j�F “ú–{’n�k�HŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶�W Vol�F 9-3Šª ”N�F 1994”N •Å�F E.43-E.48•Å ’˜ŽÒ�i˜a�j�F - ƒ^ƒCƒgƒ‹�i˜a�j�F - �´˜^�i˜a�j�F
- ƒL�[ƒ��[ƒh�i˜a�j�F - Œf�ÚŽGŽ��i‰p�j�F PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒ�i‰p�j�F Kazuyoshi KUDO, Tsutomu SASATANI, Minoru SAKAUE, Seiji SAITO, Hideki NAGUMO, Masayoshi TAKAHASHI ƒ^ƒCƒgƒ‹�i‰p�j�F 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‰p�j�F
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��[ƒh�i‰p�j�F - ‹LŽ–‹æ•ª�F - ‹æ•ª �@�@�@ˆÏˆõ‰ï˜_•¶�W