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Title

PRELIMINARY RESULTS OF PALEOSEISMOLOGIC TRENCHING ALONG THE ASTANEH FAULT

Pages

  84-93

Abstract

 The Astaneh fault with a length of more than 75 km is located in NW of DAMGHAN. Morphotectonic investigation along the Astaneh fault and left - lateral displacement in quaternary deposits shows that, Astaneh is an active fault. It is necessary to recognize paleoseismicity of Astaneh fault because, this fault is located in seismic zone of Komes HISTORICAL EARTHQUAKE with Ms=7.9 (Ambraseys & Melville, 1982). Many people (more than 45000) were killed in DAMGHAN city in Komes HISTORICAL EARTHQUAKE. In this paper, 4-5 paleo events along the Astaneh fault are presented through paleoseismological investigation.

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    APA: Copy

    SHOKRI, MOHAMMAD ALI, GHOREYSHI, MANOUCHEHR, NAZARI, HAMID, SALAMATI, REZA, TALEBIAN, M., RITZ, J.F., MOHAMMADKHANI, HOSSEIN, & SHAH PASANDZADEH, MAJID. (2009). PRELIMINARY RESULTS OF PALEOSEISMOLOGIC TRENCHING ALONG THE ASTANEH FAULT. GEOSCIENCES, 18(70), 84-93. SID. https://sid.ir/paper/31668/en

    Vancouver: Copy

    SHOKRI MOHAMMAD ALI, GHOREYSHI MANOUCHEHR, NAZARI HAMID, SALAMATI REZA, TALEBIAN M., RITZ J.F., MOHAMMADKHANI HOSSEIN, SHAH PASANDZADEH MAJID. PRELIMINARY RESULTS OF PALEOSEISMOLOGIC TRENCHING ALONG THE ASTANEH FAULT. GEOSCIENCES[Internet]. 2009;18(70):84-93. Available from: https://sid.ir/paper/31668/en

    IEEE: Copy

    MOHAMMAD ALI SHOKRI, MANOUCHEHR GHOREYSHI, HAMID NAZARI, REZA SALAMATI, M. TALEBIAN, J.F. RITZ, HOSSEIN MOHAMMADKHANI, and MAJID SHAH PASANDZADEH, “PRELIMINARY RESULTS OF PALEOSEISMOLOGIC TRENCHING ALONG THE ASTANEH FAULT,” GEOSCIENCES, vol. 18, no. 70, pp. 84–93, 2009, [Online]. Available: https://sid.ir/paper/31668/en

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