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Information Journal Paper

Title

ESTIMATION OF EARTHQUAKE MAGNITUDES USING CODA WAVE DURATION IN ZAGROS ZONE AND SOUTHWEST IN CENTRAL IRAN

Pages

  15-22

Abstract

 Amplitude and DURATION of seismic signals depend on recording distance, propagation path of the wave through different media and geology at the recording site. In addition, amplitude of recorded signals varies according to the P- and S-wave radiation patterns. Influence of these factors on seismic signals has been considered for magnitude computation in many seismic regions (e.g., Michaelson, 1990 and Eaton, 1992). Estimation of earthquake magnitude is a routine task in all seismological observatories. …

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    APA: Copy

    ASADI, S., RAHIMI, H., REZAPOUR, M., & AMIRIFARD, R.. (2017). ESTIMATION OF EARTHQUAKE MAGNITUDES USING CODA WAVE DURATION IN ZAGROS ZONE AND SOUTHWEST IN CENTRAL IRAN. JOURNAL OF THE EARTH AND SPACE PHYSICS, 43(1 ), 15-22. SID. https://sid.ir/paper/80372/en

    Vancouver: Copy

    ASADI S., RAHIMI H., REZAPOUR M., AMIRIFARD R.. ESTIMATION OF EARTHQUAKE MAGNITUDES USING CODA WAVE DURATION IN ZAGROS ZONE AND SOUTHWEST IN CENTRAL IRAN. JOURNAL OF THE EARTH AND SPACE PHYSICS[Internet]. 2017;43(1 ):15-22. Available from: https://sid.ir/paper/80372/en

    IEEE: Copy

    S. ASADI, H. RAHIMI, M. REZAPOUR, and R. AMIRIFARD, “ESTIMATION OF EARTHQUAKE MAGNITUDES USING CODA WAVE DURATION IN ZAGROS ZONE AND SOUTHWEST IN CENTRAL IRAN,” JOURNAL OF THE EARTH AND SPACE PHYSICS, vol. 43, no. 1 , pp. 15–22, 2017, [Online]. Available: https://sid.ir/paper/80372/en

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