2004”N4ŒŽ24“ú “ü‘qFŽŸ˜Yæ¶‘ÞŠ¯‹L”OƒVƒ“ƒ|ƒWƒEƒ€•j‰ê‰ï
ƒVƒ“ƒ|ƒWƒEƒ€u‹k“®—\‘ª‚ÌŒ»ó‚Æ«—ˆv
‹L”OƒVƒ“ƒ|ƒWƒEƒ€u‹k“®—\‘ª‚ÌŒ»ó‚Æ«—ˆv‚ªCƒEƒFƒXƒeƒBƒ“û·ƒzƒeƒ‹‹ž“s‚̃RƒXƒ‚ƒXƒz[ƒ‹‚ɂĊJ³‚ê‚Ü‚µ‚½B
µ‘Òu‰‰
“Œ‹ž‘åŠw’nkŒ¤‹†Š “‡è–M•F‹³Žö@’·Šú•]‰¿‚Æ‹k“®—\‘ªFŒ´—‚ÆŒ»ŽÀ‚ÌÚ“_ |
“Œ‹žH‹Æ‘åŠw‘åŠw‰@‘‡—HŠwŒ¤‹†‰È ‰ìŽO˜Y‹³Žö@’nk–hЂƋk“®—\‘ª|Žs–¯‚É–ð—§‚Â’nk“®—\‘ª’n}‚ÉŒü‚¯‚Ä| |
Joseph Fourier‘åŠw Michel Bochon‹³Žö@Variability of rupture velocity during earthquakes and its implications for strong ground motion |
URS Coporation Paul G. Somerville”ŽŽm@Characterizing earthquake rupture models for the prediction of strong ground motion |
“Á•Êu‰‰
“ü‘qFŽŸ˜Yæ¶@‹k“®Œ¤‹†‚©‚瓾‚ç‚ꂽ‹³ŒP‚Æ¡Œã‚̉ۑè |
![]() |
![]() |
“ü‘qFŽŸ˜Yæ¶‚É‚æ‚éŽïŽ|à–¾ | “Œ‹ž‘åŠw’nkŒ¤‹†Š‹³Žö@“‡è–M•Fæ¶ |
![]() |
![]() |
“Œ‹žH‹Æ‘åŠw‘åŠw‰@‘‡—HŠwŒ¤‹†‰È‹³Žö@‰ìŽO˜Yæ¶ | Joseph Fourier‘åŠw‹³Žö@Michel Bouchonæ¶ |
![]() |
![]() |
URS Corporation@Paul Somervilleæ¶ | ‰ïê‚̂悤‚· |
![]() |
![]() |
Ži‰ï‚Ìì£”Žæ¶(‹ãB‘åŠw)‚ÆŠ˜]ŽGæ¶(‹ž“s‘åŠwŒ´Žq˜FŽÀŒ±Š) | “ü‘qFŽŸ˜Yæ¶ |
![]() |
![]() |
“ü‘qFŽŸ˜Yæ¶ | ‰Ô‘©‘¡’æ(‘¡’æŽÒ‚Í‚¨ì—l‚Ì“ì‰ÆÊ‚³‚ñ) |
j‰ê‰ï
ƒVƒ“ƒ|ƒWƒEƒ€I—¹ŒãC“ü‘qæ¶‘ÞŠ¯‹L”Oj‰ê‰ï‚ªCƒEƒFƒXƒeƒBƒ“‹ž“sEû·ƒzƒeƒ‹‚Ì•ä‚̊ԂɂĊJ³‚ê‚Ü‚µ‚½B
![]() |
![]() |
’nkЊQŒ¤‹†•”–å ’†“‡³ˆ¤‹³Žö‚É‚æ‚éŠJ‰ïˆ¥ŽA | ‰ïê‚̂悤‚· |
![]() |
![]() |
—ˆ•ojŽ«F”ö’r˜a•v ‹ž“s‘åŠw‘’· | —ˆ•ojŽ«FŽR‰º‹P•v “Œ‹ž‘åŠw’nkŒ¤‹†ŠŠ’· |
![]() |
![]() |
—ˆ•ojŽ«Fˆäã˜a–ç ‹ž“s‘åŠw–hÐŒ¤‹†ŠŠ’· | ¬—Ñ–F³æ¶iŒ³‹ž“s‘åŠw—Šw•”‹³Žöj‚Ì”º‚É‚æ‚銣”t |
![]() |
![]() |
‰ïê‚̂悤‚· | ‰ïê‚̂悤‚· |
![]() |
![]() |
‰Ô‘©‘¡’æ | “ü‘qFŽŸ˜Yæ¶‚©‚ç‚̈¥ŽA |
![]() |
![]() |
’nkЊQŒ¤‹†•”–å ²“¡’‰M‹³Žö‚É‚æ‚镉ŽA | “ü‘qFŽŸ˜Yæ¶‚²•vȂ̑Þê |
> •\ކ