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Title

Khazar Fault, its s tructure and activity

Pages

  63-74

Abstract

 The Khazar Fault in the northern part of the Alborz mountains have changed the topography by making an obvious terrace in which along that the mountain drainage lines is ended where it is impossible to observe the geology s tructures due to the severe erosion and massive vegetation. The simultaneous s trike-slip and thrus t movements parallel to the Alborz mountain chain shows that the deformation in this range is the result of the oblique shortening. This deformation indicates an sinis tral transpression sys tem in the northern ridge of this mountain chain along the Khazar Fault. The progressive activity of the Khazar Fault has caused the fault segments, with s trike-slip mechanisms, originating from it. These faults almos t aren’ t so long and are ended to some fractures in their southern range. The northern ridge of Alborz mountain range is controlled by their s trike-slip displacement and the Khazar Fault.

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    APA: Copy

    RASHIDI, AHMAD, & Hessami Azar, Khaled. (2018). Khazar Fault, its s tructure and activity. TECTONICS, 2(7 ), 63-74. SID. https://sid.ir/paper/384427/en

    Vancouver: Copy

    RASHIDI AHMAD, Hessami Azar Khaled. Khazar Fault, its s tructure and activity. TECTONICS[Internet]. 2018;2(7 ):63-74. Available from: https://sid.ir/paper/384427/en

    IEEE: Copy

    AHMAD RASHIDI, and Khaled Hessami Azar, “Khazar Fault, its s tructure and activity,” TECTONICS, vol. 2, no. 7 , pp. 63–74, 2018, [Online]. Available: https://sid.ir/paper/384427/en

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