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Title

DETERMINATION OF CODA WAVE QUALITY FACTOR IN THE NORTH-WEST OF THE IRANIAN PLATEAU

Pages

  271-280

Abstract

 The energy of a seismic wave decays while passing througha “real” medium such as the earth which is not completely elastic. Scattering and ATTENUATION of high-frequency seismic waves are substantial parameters to quantify and to physically characterize the earth medium and from which useful information on medium properties can be inferred. The CODA WAVES in seismograms are one of the most prominent observations supporting the existence random heterogeneities in the earth. Determination of source parameters must take into account the proper ATTENUATION characteristic of the wave path. Moreover, it is essential for seismic risk studies and seismic hazard assessment, and consequently for seismic risk mitigation and engineering seismology. ...

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    APA: Copy

    NAGHAVI, M., RAHIMI, H., & MORADI, A.. (2016). DETERMINATION OF CODA WAVE QUALITY FACTOR IN THE NORTH-WEST OF THE IRANIAN PLATEAU. GEOSCIENCES, 25(100), 271-280. SID. https://sid.ir/paper/31685/en

    Vancouver: Copy

    NAGHAVI M., RAHIMI H., MORADI A.. DETERMINATION OF CODA WAVE QUALITY FACTOR IN THE NORTH-WEST OF THE IRANIAN PLATEAU. GEOSCIENCES[Internet]. 2016;25(100):271-280. Available from: https://sid.ir/paper/31685/en

    IEEE: Copy

    M. NAGHAVI, H. RAHIMI, and A. MORADI, “DETERMINATION OF CODA WAVE QUALITY FACTOR IN THE NORTH-WEST OF THE IRANIAN PLATEAU,” GEOSCIENCES, vol. 25, no. 100, pp. 271–280, 2016, [Online]. Available: https://sid.ir/paper/31685/en

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