Attenuation of P and S waves in Western part of Iran

Author:

Amiri Fard R1,Javan Doloei G1,Rahimi H2,Farrokhi M3

Affiliation:

1. International Institute of Earthquake Engineering and Seismology, Tehran, Iran

2. Institute of Geophysics, University of Tehran, Tehran, Iran

3. Dept. of Physics, University of Hormozgan, Bandar Abbas, Iran

Funder

International Institute of Earthquake Engineering and Seismology

Institute for Advanced Studies in Basic Sciences

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference104 articles.

1. Numerical and experimental study of turbulent impinging twin-jet flow;Abdel-Fattah;Exp. Therm. Fluid Sci.,2007

2. Crustal structure of northwest Zagros (Kermanshah) and Central Iran (Yazd and Isfahan) using teleseismic PS converted phases;Afsari;J. Seismol.,2011

3. Analysis of the seismic coda of local earthquakes as scattered waves;Aki;J. geophys. Res.,1969

4. Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz, Physics of the Earth and Planetary Interiors;Aki,1980

5. Source and scatering effects on the spectra of small local earthquakes;Aki;Bull. seism. Soc. Am.,1981

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