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Information Journal Paper

Title

COMPARISON BETWEEN SHEAR WAVE VELOCITY IN BAM AREA AND DESTROYED AREA IN 26TH DEC 2003 EARTHQUAKE

Pages

  109-118

Abstract

 In soft soil SURFACE LAYER the intensity of seismic waves are more and it causes more DESTRUCTION. On the other hand in geophysical aspect, for estimation of softness or hardness of layers there is a suitable scale that named SHEAR WAVE velocity.In this research, SHEAR WAVE velocity in the first layer is calculated by 80 REFRACTION seismic profiles in BAM. This area is zoned by SHEAR WAVE velocity. Destroyed map of the 26th of Dec 2003 earthquake that has been immediately prepared. is compared with the SHEAR WAVE velocity in the first layer and significant results achieved. as we know in low velocity zones DESTRUCTION must be more and vice versa, but somewhere that is not happen, as we guess it is for kind of construction, distance to fault, depth of bed rock and etc.

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  • Cite

    APA: Copy

    NARAGHI ARAGHI, NOOSHIN, HASHEMI TABATABI, SAEED, & BEITOLLAHI, ALI. (2010). COMPARISON BETWEEN SHEAR WAVE VELOCITY IN BAM AREA AND DESTROYED AREA IN 26TH DEC 2003 EARTHQUAKE. JOURNAL OF THE EARTH, 5(2), 109-118. SID. https://sid.ir/paper/193017/en

    Vancouver: Copy

    NARAGHI ARAGHI NOOSHIN, HASHEMI TABATABI SAEED, BEITOLLAHI ALI. COMPARISON BETWEEN SHEAR WAVE VELOCITY IN BAM AREA AND DESTROYED AREA IN 26TH DEC 2003 EARTHQUAKE. JOURNAL OF THE EARTH[Internet]. 2010;5(2):109-118. Available from: https://sid.ir/paper/193017/en

    IEEE: Copy

    NOOSHIN NARAGHI ARAGHI, SAEED HASHEMI TABATABI, and ALI BEITOLLAHI, “COMPARISON BETWEEN SHEAR WAVE VELOCITY IN BAM AREA AND DESTROYED AREA IN 26TH DEC 2003 EARTHQUAKE,” JOURNAL OF THE EARTH, vol. 5, no. 2, pp. 109–118, 2010, [Online]. Available: https://sid.ir/paper/193017/en

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