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Information Journal Paper

Title

HARACTERISTICS OF SEISMICITY IN SILAKHOR BROJERD AREA BASED ON EARTHQUAKES OF IIBES TEMPORARY SEISMIC NET

Pages

  697-716

Abstract

 Silakhor Brojerd area is between high Zagros zone and Sanandaj-Sirjan zone and is one of the seismic areas, with high frequency of occurrence and medium magnitude and sometimes high magnitude, in Iran. Area of maximum destruction and fault plane solutions show a NW-SE trend. Observation of aftershock distribution, caused by earthquake of 1384/2/31, on the region delineated that most of them have occurred in the epicenter area of the main shock, on Ghale-Hatam fault. Also most of aftershocks, caused by earthquake of 1385/1/13 in Brojerd, have occurred in epicenter area of the main shock on Doroud fault. Moreover, focal mechanisms of earthquakes, are right lateral strike-slip with some normal or reverse dip-slip. These different solutions, next to each others indicate partitioning in this area of Zagros.

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    • Cite

    APA: Copy

    SHAHRABI, T., & JAVAN DOULOUEI, GH.. (2010). HARACTERISTICS OF SEISMICITY IN SILAKHOR BROJERD AREA BASED ON EARTHQUAKES OF IIBES TEMPORARY SEISMIC NET. JOURNAL OF ENGINEERING GEOLOGY, 3(2), 697-716. SID. https://sid.ir/paper/186285/en

    Vancouver: Copy

    SHAHRABI T., JAVAN DOULOUEI GH.. HARACTERISTICS OF SEISMICITY IN SILAKHOR BROJERD AREA BASED ON EARTHQUAKES OF IIBES TEMPORARY SEISMIC NET. JOURNAL OF ENGINEERING GEOLOGY[Internet]. 2010;3(2):697-716. Available from: https://sid.ir/paper/186285/en

    IEEE: Copy

    T. SHAHRABI, and GH. JAVAN DOULOUEI, “HARACTERISTICS OF SEISMICITY IN SILAKHOR BROJERD AREA BASED ON EARTHQUAKES OF IIBES TEMPORARY SEISMIC NET,” JOURNAL OF ENGINEERING GEOLOGY, vol. 3, no. 2, pp. 697–716, 2010, [Online]. Available: https://sid.ir/paper/186285/en

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