ŒfÚŽGŽi˜ajF | “ú–{’nkHŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶W |
VolF | 11Šª |
”NF |
2002”N
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•ÅF |
139-144•Å
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’˜ŽÒi˜ajF |
_“c@Ž‹vC•‘º@‰ë”VC‰F²”ü@—´•v
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ƒ^ƒCƒgƒ‹i˜ajF |
k“xƒf[ƒ^‚ð—p‚¢‚½“ŒŠCE“ìŠC’nk‚ÌkŒ¹“Á«‚Ì„’è
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´˜^i˜ajF |
-
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ƒL[ƒ[ƒhi˜ajF |
k“x•ª•zCƒAƒXƒyƒŠƒeƒBC“™‰¿kŒ¹‹——£C‚·‚ׂ蕪•zCƒCƒ“ƒo[ƒWƒ‡ƒ“‰ðÍ
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ŒfÚŽGŽi‰pjF |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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’˜ŽÒi‰pjF |
Katsuhisa Kanda, Masayuki Takemura, Tatsuo Usami
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ƒ^ƒCƒgƒ‹i‰pjF |
FAULT CHARACTERISTICS OF THE TOKAI & NANKAI EARTHQUAKES BASED ON SEISMIC INTENSITY DATA
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´˜^i‰pjF |
The least square sense analysis is carried out to identify optimized energy distribution on the fault of the Tokai and Nankai earthquakes of Hoei, Ansei and Showa so as to minimize the discrepancy between observed and evaluated seismic intensity. The seismic intensity at each site is evaluated from the attenuation regression formula with equivalent hypocentral distance, magnitude and relative intensity index representing local site amplification. It is indicated that the high energy portions called asperities tend to locate in the Kochi and Wakayama offing for the Nankai earthquake, and to locate in the Sea of Kumano and Enshu, and in the center of Shizuoka for the Tokai and Tonakan earthquake.
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ƒL[ƒ[ƒhi‰pjF |
seismic intensity, asperity, equivalent hypocentral distance, slip distribution, inversion analysis
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‹LŽ–‹æ•ªF |
-
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‹æ•ªF |
ˆÏˆõ‰ï˜_•¶W |