@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W VolF 9-1Šª ”NF 1994”N •ÅF 403-408•Å ’˜ŽÒi˜ajF “Œ@’å¬CŽÅ@—Ǻ ƒ^ƒCƒgƒ‹i˜ajF ‚P‚X‚X‚R”N–kŠC“¹“켉«’nk‚Ì—]kŠÏ‘ª ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Sadanori HIGASHI, Yoshiaki SHIBA ƒ^ƒCƒgƒ‹i‰pjF STRONG MOTION OBSERVATION OF THE AFTERSHOCKS OF THE 1993 HOKKAIDO-NANSEI-OKI EARTHQUAKE ´˜^i‰pjF
We observed aftershocks of the 1993 Hokkaido-Nansei-Oki Earthquake at temporary stations, OKS and STN. From the spectral ratios of the events to a standard one in three event groups, we found that the stress drop varied by the factor of two between the events of the same magnitude, and that stress drop increased with magnitude in a group. Complex polarization filter was applied to the accelerograms for the major aftershock event(M6.5). From the polarization analysis we found the radiation pattern of the event caused the difference of the strong motion between OKS and STN. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W