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Information Journal Paper

Title

DETERMINATION OF SOUTH MASHHAD FAULT ZONE USING MICRO TREMORS

Pages

  17-30

Abstract

 In This study, the Href="/search/paper/MICROTREMORE/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank">MICROTREMORE data were used for recognition and mapping the SOUTH MASHHAD FAULT zone. For this, in 27 points and 5 profiles normal to the mountain of south Mashhad single stations Href="/search/paper/MICROTREMORE/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank">MICROTREMORE data were measured and by the dominant frequency are estimated using the spectral ratio (HVSR) method. Then Map of the period and its variations drawn In the Highlands south of the city and the Stations with sudden change in the amount of frequency are marked on the map. Moreover, anisotropy of dominant frequency and amplification in all stations are checked and the station with High anisotropies of amplification marked. Finally, by comparing the results of both methods with reviews the area borehole and evidence of fault activity on aerial photographs, location of Mashhad fault zone are proposed. The results Have good agreements with site evidence and aerial photo interpretation.

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    APA: Copy

    ZAHANI GHAEINI, M., HAFEZI MOGHADDAS, N., & GHAFOORI, M.. (2016). DETERMINATION OF SOUTH MASHHAD FAULT ZONE USING MICRO TREMORS. ENGINEERING GEOLOGY, 8(3-4), 17-30. SID. https://sid.ir/paper/137655/en

    Vancouver: Copy

    ZAHANI GHAEINI M., HAFEZI MOGHADDAS N., GHAFOORI M.. DETERMINATION OF SOUTH MASHHAD FAULT ZONE USING MICRO TREMORS. ENGINEERING GEOLOGY[Internet]. 2016;8(3-4):17-30. Available from: https://sid.ir/paper/137655/en

    IEEE: Copy

    M. ZAHANI GHAEINI, N. HAFEZI MOGHADDAS, and M. GHAFOORI, “DETERMINATION OF SOUTH MASHHAD FAULT ZONE USING MICRO TREMORS,” ENGINEERING GEOLOGY, vol. 8, no. 3-4, pp. 17–30, 2016, [Online]. Available: https://sid.ir/paper/137655/en

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