Figure 8. Comparison of the spectral responses of the three component acceleration records of the Nov. 23 Gölyaka earthquake on the Düzce Plain, which consists of Quaternary thick alluvium. The spectral response curves recommended for the same points in the Turkish Building Earthquake Code (TBEC, 2018) on the response curves are shown with thick black lines. The high value observed between the T(s):1s and T(s):2s periods in the spectrum obtained from the 8102 coded recorder exceeded the recommended value in TBEC (2018) by 40%. Credit: Haluk Eyidoğan

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Figure 8. Comparison of the spectral responses of the three component acceleration records of the Nov. 23 Gölyaka earthquake on the Düzce Plain, which consists of Quaternary thick alluvium. The spectral response curves recommended for the same points in the Turkish Building Earthquake Code (TBEC, 2018) on the response curves are shown with thick black lines. The high value observed between the T(s):1s and T(s):2s periods in the spectrum obtained from the 8102 coded recorder exceeded the recommended value in TBEC (2018) by 40%. Credit: Haluk Eyidoğan

Figure 8. Comparison of the spectral responses of the three component acceleration records of the Nov. 23 Gölyaka earthquake on the Düzce Plain, which consists of Quaternary thick alluvium. The spectral response curves recommended for the same points in the Turkish Building Earthquake Code (TBEC, 2018) on the response curves are shown with thick black lines. The high value observed between the T(s):1s and T(s):2s periods in the spectrum obtained from the 8102 coded recorder exceeded the recommended value in TBEC (2018) by 40%. Credit: Haluk Eyidoğan

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