Category Archives: ラクイラ地震


ラクイラ地震の分析 L’AQUILA-V.ATERNO-CENTRO VALLE M5.8 LAquila Italy Earthquake of 06 Apr 2009 Station:L’AQUILA-V.ATERNO-CENTRO VALLE. 42.377N,13.344E,4.8km from EpicenterPDF Document:Fourier Amplitude Spectrum:-10(Hz) URL MD5 258b1fee8cdbe6c4ee9da83bc84c04fbPDF Document:H/V Spectral Ratio URL MD5 fa2af184ce23fb5cbe893dd234405052PDF Document:Maximum Response by Building Height.Structure:Reinforced Concrete URL MD5 0d9b58ec9ad12e53e1e7a72f863305e2PDF Document:Sa-Sd Curve.Sa:Maximum Absolute Acceleration Response,Sd:Maximum Relative Displacement Response URL MD5 b187291b424fc9b11b1f28c865bdaa62
View Larger Map Reference [1] [2]大崎順彦:『新・地震動のスペクトル解析入門』,鹿島出版会,1994 [3]日本建築学会:『建築物の減衰』,丸善,2000 [4]Yukio Tamura:『Damping in Buildings』 [5]Nelson PULIDO, Toru SEKIGUCHI, Gaku SHOJI , Jorge ALBA, Fernando LAZARES, Taiki SAITO:『Earthquake Source Process and Strong Ground Motions of the 2010 Chile Mega-Earthquake』 [6]Patricio Poblete:『Surviving the 8.8 Richter Chilean Earthquake of 27 Feb 2010 3:34am』 [7] [8] [9] [10] ・PDF作成日はドキュメントの左下、「Document ID No.」の前から8桁に記しています。例 20120302→2012年3月2日. ・Fourier amplitude spectrum is calculated by Fast Fourier transform(FFT). ・Fourier amplitude spectrum is calculated with no noise filtering. ・Maximum Response is calculated with no noise filtering. ・Average(gal) in the document is the value after minus offset. ・1G=980.665cm/s^2 ※Caution:Calculated directly from original uncorrected accelerogram data minus offset. ※Offset is the average of all original uncorrected accelerogram data.