Estimation of Quality Factor (Qβ) Using Accelerograms of Ahar-Varzaghan Earthquakes, Northwestern Iran

Authors

  • Majid Mahood Earthquake Prediction Center, International Institute of Earthquake Engineering and Seismology, Tehran
  • Saman Amiri Earthquake Prediction Center, International Institute of Earthquake Engineering and Seismology, Tehran

DOI:

https://doi.org/10.15273/ijge.2017.03.008

Keywords:

Attenuation, Qβ (f), Inversion, Ahar-Varzaghan Earthquake, NW-Iran

Abstract

High-frequency strong-motion data of two recent major earthquakes in the Ahar-Varzaghan region, Northwestern Iran, have been used to determine shear-wave quality factor (Qβ (f)) and seismic source parameters. Data from a local array of 12 stations, two main shocks (Ahar-Varzaghan doublet earthquakes (Mw 6.4 and 6.3) on August 11, 2012), and 38 aftershocks of magnitude 4.1 – 5 were analyzed. The classic Brune model is used to predict the shape of the source spectrum and to provide scaling relationships between spectral and source parameters. In order to obtain reliable estimates of the source spectrum, the effects of attenuation need to be estimated and corrected. By using an inversion algorithm in this work, an average relation in the form Qβ = (114 ± 21) f (0.90  ±  0.07) is obtained. The best fit theoretical spectrum provides final values of source parameters, i.e. seismic moment Mo and corner frequency fc as 3.19 à— 1025 dyne cm and 0.69 Hz, respectively, for the first event. Obtained Q(f) relationship suggests a low Qo value (< 200) and a high n value (> 0.8) for high heterogeneous, tectonically and seismically active regions.

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Published

2017-08-21

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Section

Articles