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Information Journal Paper

Title

THRUST MECHANISM OF NORTH LIMB OF GARMABDAR ANTICLINE (CENTRAL ALBORZ)

Pages

  27-33

Abstract

GARMABDAR ANTICLINE, located between 51o 30’-51o 45’ eastern longitudes and 35o 55’-36o northern latitude, with an area of 220 Km2 and E-W axis, is one of the STRUCTURAL SUB-ZONEs in the south of central Alborz range. GARMABDAR ANTICLINE, situated between Garmabdar overthrust in north and Mosha fault in south component of Paleozoic and Mesozoic older formation. Field mapping accompanied by structural interpretation of the study area shows that THRUST FAULT with minor strike component that toward north and south (back thrust), are the main structures that control deformation in the sub-zones. kinematic analysis shows that it was developed by propagation of THRUST FAULT. Therefore, it was classified as fault propagation fold. The THRUST SEQUENCE of these study area is correlated with FORWARD-BREAKING SEQUENCE.

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    APA: Copy

    SHEIKH MAHBOOBI, SARA, ALMASIAN, MAHMOUD, & ABBASI, MOHAMMADREZA. (2007). THRUST MECHANISM OF NORTH LIMB OF GARMABDAR ANTICLINE (CENTRAL ALBORZ). JOURNAL OF THE EARTH, 2(2), 27-33. SID. https://sid.ir/paper/193023/en

    Vancouver: Copy

    SHEIKH MAHBOOBI SARA, ALMASIAN MAHMOUD, ABBASI MOHAMMADREZA. THRUST MECHANISM OF NORTH LIMB OF GARMABDAR ANTICLINE (CENTRAL ALBORZ). JOURNAL OF THE EARTH[Internet]. 2007;2(2):27-33. Available from: https://sid.ir/paper/193023/en

    IEEE: Copy

    SARA SHEIKH MAHBOOBI, MAHMOUD ALMASIAN, and MOHAMMADREZA ABBASI, “THRUST MECHANISM OF NORTH LIMB OF GARMABDAR ANTICLINE (CENTRAL ALBORZ),” JOURNAL OF THE EARTH, vol. 2, no. 2, pp. 27–33, 2007, [Online]. Available: https://sid.ir/paper/193023/en

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