Abstract – The strong ground motions recorded during the 2002 Avaj earthquake have been used to estimate S wave attenuation, Qβ, and spectral decay parameter, κ, for the Avaj region. Qβ for shear wave is estimated as a function of frequency in the range of 0.6- 18 Hz. The results show that Qβ increases with frequency in the form of Qβ=62.7 f 0.9. Our estimates are within the estimated range for different parts of the world for Qo and n. The spectral decay parameter, κ, has been estimated from the high frequency of the spectra. The dependence of κ on the epicenteral distance for the Avaj region is also found
Distinguishing source, path, and site responses from S-wave displacement spectra recorded by the Ind...
In this study, the attenuation of coda waves has been estimated in the western part of Iran plateau ...
Abstract We calculated the spectral decay parameter (κ) in the southern Basin and Range province, us...
A nonparametric generalized inversion technique (GIT) has been used to derive attenuation characteri...
We determined a set of empirical functions that describe the spectral amplitude decay of S-waves wit...
We comprehensively analyze attenuation factor in Kopili region and its neighboring area. Correspondi...
The large number of strong motion data from the national network of strong motion Iran (NSMNI) motiv...
At high frequencies f the spectrum of S-wave accelerations is characterized by a trend of exponentia...
Among important parameters in simulation of earthquake data in high frequencies are the high frequen...
We analyze S-wave spectra from strong motion seismograms observed at the rock and sedimentary sites....
Abstract The frequency-dependent attenuations of P and S waves in the crust be-neath Bhuj are estima...
Abstract The S-wave Fourier amplitude spectra from the strong-motion network data in the Himachal re...
In the present study the attenuation mechanism of seismic wave energy in and around the source area ...
The frequency-dependent attenuation of shear waves in the crust is estimated by using two different ...
Empirical scaling equations for Fourier amplitude spectra of strong ground motion are used to descri...
Distinguishing source, path, and site responses from S-wave displacement spectra recorded by the Ind...
In this study, the attenuation of coda waves has been estimated in the western part of Iran plateau ...
Abstract We calculated the spectral decay parameter (κ) in the southern Basin and Range province, us...
A nonparametric generalized inversion technique (GIT) has been used to derive attenuation characteri...
We determined a set of empirical functions that describe the spectral amplitude decay of S-waves wit...
We comprehensively analyze attenuation factor in Kopili region and its neighboring area. Correspondi...
The large number of strong motion data from the national network of strong motion Iran (NSMNI) motiv...
At high frequencies f the spectrum of S-wave accelerations is characterized by a trend of exponentia...
Among important parameters in simulation of earthquake data in high frequencies are the high frequen...
We analyze S-wave spectra from strong motion seismograms observed at the rock and sedimentary sites....
Abstract The frequency-dependent attenuations of P and S waves in the crust be-neath Bhuj are estima...
Abstract The S-wave Fourier amplitude spectra from the strong-motion network data in the Himachal re...
In the present study the attenuation mechanism of seismic wave energy in and around the source area ...
The frequency-dependent attenuation of shear waves in the crust is estimated by using two different ...
Empirical scaling equations for Fourier amplitude spectra of strong ground motion are used to descri...
Distinguishing source, path, and site responses from S-wave displacement spectra recorded by the Ind...
In this study, the attenuation of coda waves has been estimated in the western part of Iran plateau ...
Abstract We calculated the spectral decay parameter (κ) in the southern Basin and Range province, us...