@ ŒfÚŽGŽi˜ajF “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W VolF 9-1Šª ”NF 1994”N •ÅF 421-426•Å ’˜ŽÒi˜ajF ’†“‡@N‰ëC@¡–{@‹I’jC@‰`–{@F‹vC@’O‘ò@NC@“n•”@ˆê—²C@“¡–{@ˆê˜Y ƒ^ƒCƒgƒ‹i˜ajF ‚P‚X‚X‚Q”N“Œ‹ž˜p’nk‚É‚æ‚鉡•lŽsEŽOa”¼“‡‚Ìk“x•ª•z ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF - ŒfÚŽGŽi‰pjF PROCEEDINGS OF THE JAPAN EARTHQUAKE ENGINEERING SYMPOSIUM ’˜ŽÒi‰pjF Yasumasa NAKAJIMA, Norio ABEKI, Takahisa ENOMOTO, Yasusi TANZAWA, Kazutaka WATAMABE, Ichiro FUJIMOTO ƒ^ƒCƒgƒ‹i‰pjF ON THE SEISMIC INTENSITY DISTRIBUTION IN YOKOHAMA CITY AND MIURA PENINSULA, CAUSED BY THE 1992 TOXYO BAY EARTHQUAKE ´˜^i‰pjF
Authors carried out questionnaire survey for the estimation of seismic intensity (JMA Intensity Scale) in YOKOHAMA CITY and MIURA PENINSULA, caused by the 1992 February 2nd Tokyo Bay Earthquake. And the objects of this paper are to make clear the seismic intensity distribution in target area and discuss the relation between the effects of surface geology and the seismic intensity. As the results, authors found the area highly influenced by the local soil conditions and were able to make clear the characteristics of seismic intensity distribution in this surveyed area. ƒL[ƒ[ƒhi‰pjF - ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W