2007
DOI: 10.1016/j.engstruct.2006.09.022
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Site dependent response spectra and analysis of the characteristics of the strong ground motion due to the 1999 Duzce earthquake in Turkey

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Cited by 6 publications
(2 citation statements)
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“…This spectral amplification coefficient is determined from the response spectrum or normalized response spectrum curve of bedrock seismic motion at sites S A and S B (Figure 13). The normalized response spectrum can be interpreted as amplification factor of response and is obtained by dividing the pseudo spectral acceleration by peak ground acceleration (PGA) (Bakir et al, 2007). The ratio between spectral amplification coefficients of sites S A and S B is equal to 1.83 which is in good agreement with the ratio between recorded free field motions.…”
Section: Discussionsupporting
confidence: 58%
“…This spectral amplification coefficient is determined from the response spectrum or normalized response spectrum curve of bedrock seismic motion at sites S A and S B (Figure 13). The normalized response spectrum can be interpreted as amplification factor of response and is obtained by dividing the pseudo spectral acceleration by peak ground acceleration (PGA) (Bakir et al, 2007). The ratio between spectral amplification coefficients of sites S A and S B is equal to 1.83 which is in good agreement with the ratio between recorded free field motions.…”
Section: Discussionsupporting
confidence: 58%
“…Normalized response spectra of each component of the two stations were computed for various damping ratio (2, 5 and 10%). These normalized response spectra can be interpreted as amplification factors of response and are obtained by dividing the pseudo spectral acceleration (PSA), pseudo spectral velocity (PSV) and spectral displacement (SD) by PGA, PGV and PGD, respectively (Bakir et al, 2007).…”
Section: Effect Of Damping Ratio On Response Spectramentioning
confidence: 99%