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VolF11Šช
”NF 2002”N
•ลF 2265-2270•ล
’˜Žาi˜ajF โV“c@~CKhosrow T. ShabestariCผ‰ช@นŽuCŽR่@•ถ—Y
ƒ^ƒCƒgƒ‹i˜ajF ’นŽๆŒงผ•”’nk‹y‚ัŒ|—\’nk‚ฬŒv‘ชk“x‚ฬ‹๓Šิ•ช•z„’่
ด˜^i˜ajF -
ƒL[ƒ[ƒhi˜ajF Œv‘ชk“xC‹——ฃŒธŠŽฎC‹๓Šิ•ช•zCƒNƒŠƒbƒMƒ“ƒOC2000 ”N’นŽๆŒงผ•”’nkC2001 ”NŒ|—\’nk
ŒfฺŽGŽi‰pjF THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
’˜Žาi‰pjF Jun Saita, Khosrow T. Shabestari, Masashi Matsuoka, Fumio Yamazaki
ƒ^ƒCƒgƒ‹i‰pjF ESTIMATION OF SPATIAL DISTRIBUTION OF JMA SEISMIC INTENSITY FOR THE 2000 TOTTORI-KEN SEIBU AND 2001 GEIYO EARTHQUAKES
ด˜^i‰pjF Strong motion indices such as the instrumental JMA seismic intensity provide important information in earthquake emergency management. Because observed seismic motion is strongly affected by site response characteristics, some estimation procedures are necessary to obtain the spatial distributions of these indices. In this study the applicability of the nationwide proposed GIS-based soil amplification ratios have been examined for the October 6, 2000 Tottori-ken Seibu and the March 24, 2001 Geiyo earthquakes. For the two events a relatively good correlation between the observed and estimated ground motion indices are observed.
ƒL[ƒ[ƒhi‰pjF JMA Seismic Intensity, Attenuation relationship, Spatial distribution, Kriging, 2000 Tottori-ken Seibu Earthquake, 2001 Geiyo Earthquake
‹LŽ–‹ๆ•ชF -
‹ๆ•ชF ˆฯˆ๕‰๏˜_•ถW