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Information Journal Paper

Title

Crustal velocity structure and Moho discontinuity depth in northeast of Iran

Pages

  251-265

Abstract

 Crustal velocity structure beneath four broadband seismic stations located in Northeast of Iran, including Shahrood (SHRO) and Maraveh Tappeh (MRVT) stations set up by Iran National Seismic Network (INSN) and Sabzevar (SZBV) and Jarkhoshk (JRKH) stations set up by Iranian Seismology Center (IRSC), have been investigated by Joint Inversion of P Receiver Function and Rayleigh wave phase and group velocity dispersion curves. A three-year teleseismic data (2012-2014) with epicentral distance of 25o-90o and magnitude more than 5. 5 have been used to determine the Receiver Functions by iterative deconvolution in time domain proposed by Ligorria and Ammon (1999). Iterative deconvolution in time domain to determine the Receiver Functions are more stable with noisy data in comparison to frequency domain. The fundamental mode of Rayleigh wave group and phase velocity dispersion curves have been provided by the study on the structure of crust and upper mantle of the Iranian Plateau for the period interval of 10-100 seconds made by Rahimi (2010). ...

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    • Cite

    APA: Copy

    NASRABADI, AFSANEH, SEPAHVAND, MOHAMMAD REZA, & Limochi, Zahra. (2019). Crustal velocity structure and Moho discontinuity depth in northeast of Iran. JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS, 4(2 ), 251-265. SID. https://sid.ir/paper/268580/en

    Vancouver: Copy

    NASRABADI AFSANEH, SEPAHVAND MOHAMMAD REZA, Limochi Zahra. Crustal velocity structure and Moho discontinuity depth in northeast of Iran. JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS[Internet]. 2019;4(2 ):251-265. Available from: https://sid.ir/paper/268580/en

    IEEE: Copy

    AFSANEH NASRABADI, MOHAMMAD REZA SEPAHVAND, and Zahra Limochi, “Crustal velocity structure and Moho discontinuity depth in northeast of Iran,” JOURNAL OF RESEARCH ON APPLIED GEOPHYSICS, vol. 4, no. 2 , pp. 251–265, 2019, [Online]. Available: https://sid.ir/paper/268580/en

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