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Information Journal Paper

Title

STRUCTURAL EVIDENCE OF CHANGES IN TECTONIC REGIME FROM COMPRESSIONAL STRESS TO COMPRESSION-SHEAR STRESS IN SOUTHEAST OF THE GAVKHUNI (KHUSHAB REGION)

Pages

  197-212

Abstract

 The area under investigation is located in the eastern part of the central Iranian microcontinent. By studying various structures such as faults and folds, the changes of tectonic regime from Cretaceous to Quaternary are studied. In this paper, attempts have been made, to understand the process of convergent and compression predominance to shear stress. The Cretaceous Ophiolitic rocks, Eocene-Oligocene volcanic rocks and Travertine deposits are outcropped. The remnants of sheared oceanic lithosphere, together with double plunge folds and strike-slip faults are suitable indicators to understand the change of tectonic regime in this region.

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    Cite

    APA: Copy

    MAGHSOUDI, MEYSAM, GHORASHI, MANOOCHEHR, & NEZAM POUR, MOHAMAD HADI. (2012). STRUCTURAL EVIDENCE OF CHANGES IN TECTONIC REGIME FROM COMPRESSIONAL STRESS TO COMPRESSION-SHEAR STRESS IN SOUTHEAST OF THE GAVKHUNI (KHUSHAB REGION). JOURNAL OF THE EARTH, 7(24), 197-212. SID. https://sid.ir/paper/193010/en

    Vancouver: Copy

    MAGHSOUDI MEYSAM, GHORASHI MANOOCHEHR, NEZAM POUR MOHAMAD HADI. STRUCTURAL EVIDENCE OF CHANGES IN TECTONIC REGIME FROM COMPRESSIONAL STRESS TO COMPRESSION-SHEAR STRESS IN SOUTHEAST OF THE GAVKHUNI (KHUSHAB REGION). JOURNAL OF THE EARTH[Internet]. 2012;7(24):197-212. Available from: https://sid.ir/paper/193010/en

    IEEE: Copy

    MEYSAM MAGHSOUDI, MANOOCHEHR GHORASHI, and MOHAMAD HADI NEZAM POUR, “STRUCTURAL EVIDENCE OF CHANGES IN TECTONIC REGIME FROM COMPRESSIONAL STRESS TO COMPRESSION-SHEAR STRESS IN SOUTHEAST OF THE GAVKHUNI (KHUSHAB REGION),” JOURNAL OF THE EARTH, vol. 7, no. 24, pp. 197–212, 2012, [Online]. Available: https://sid.ir/paper/193010/en

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