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Information Journal Paper

Title

ATTENUATION OF P AND S WAVES IN MASHHAD AREA

Pages

  21-35

Abstract

 In this study, the frequency dependence of P and S wave’s attenuation are determined in terms of Q-1p and Q-1s in MASHHAD AREA. The local seismic data used in this analysis are come from 10 seismic stations, installed in the area during this study. The EXTENDED CODA NORMALIZATION METHOD has been used in this research. The analysis shows the FREQUENCY DEPENDENCE OF ATTENUATION in MASHHAD AREA. The Q-1p decrease from 0.01258±0.005034 at 1.5 Hz to 0.000863±0.000414at 24.0 Hz and Q-1s decrease from 0.008019±0.004359 at 1.5 Hz to 0.000352±0.000314 at 24.0 Hz. Using the regression methods we have fined the following relations:Q-1p (f) = (0.0162±0.0106) f (-0.9198±0.2446) Q-1s (f) = (0.0136±0.0110) f (-1.1868±0.3976)

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    APA: Copy

    NOUROUZI, GH.R., GHAFOURI ASHTIANI, M., JAVAN DOULOUEI, GH., & MOKHTARI, MOHAMMAD. (2008). ATTENUATION OF P AND S WAVES IN MASHHAD AREA. IRANIAN JOURNAL OF GEOPHYSICS, 1(1), 21-35. SID. https://sid.ir/paper/133801/en

    Vancouver: Copy

    NOUROUZI GH.R., GHAFOURI ASHTIANI M., JAVAN DOULOUEI GH., MOKHTARI MOHAMMAD. ATTENUATION OF P AND S WAVES IN MASHHAD AREA. IRANIAN JOURNAL OF GEOPHYSICS[Internet]. 2008;1(1):21-35. Available from: https://sid.ir/paper/133801/en

    IEEE: Copy

    GH.R. NOUROUZI, M. GHAFOURI ASHTIANI, GH. JAVAN DOULOUEI, and MOHAMMAD MOKHTARI, “ATTENUATION OF P AND S WAVES IN MASHHAD AREA,” IRANIAN JOURNAL OF GEOPHYSICS, vol. 1, no. 1, pp. 21–35, 2008, [Online]. Available: https://sid.ir/paper/133801/en

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