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Title

ANALYSIS OF THE MESOSCOPIC BRITTLE AND DUCTILE-BRITTLE STRUCTURES IN THE METAMORPHIC AREA OF SOUTHEASTERN EGHLID

Pages

  173-180

Abstract

 The study area, located in 40 km southeast of Eghlid town, is a metamorphozed terrain situated between the EGHLID FAULT and the Zagros Mai Thrust and is a part of the southeastern SANANDAJ-SIRJAN Zone. The area consists of the highly deformed rocks which have been emerging clearly in dextral shear zones. Mesoscopic scale analysis carried out for determining the paleostress directions and deformation history of the area. Thus MESOSCOPIC FAULTs, JOINTs and VEINs were measured and analyzed based on the field measurements and statistical methods. Then fitting structural models were presented for each of them. Furthermore, formation ages of the structures were considered based on relative time scaleAccording to the results, it can be concluded that two different deformation phases were effective in formation of the analyzed structures.

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    Cite

    APA: Copy

    ARFANIA, R.. (2012). ANALYSIS OF THE MESOSCOPIC BRITTLE AND DUCTILE-BRITTLE STRUCTURES IN THE METAMORPHIC AREA OF SOUTHEASTERN EGHLID. GEOSCIENCES, 21(82), 173-180. SID. https://sid.ir/paper/32519/en

    Vancouver: Copy

    ARFANIA R.. ANALYSIS OF THE MESOSCOPIC BRITTLE AND DUCTILE-BRITTLE STRUCTURES IN THE METAMORPHIC AREA OF SOUTHEASTERN EGHLID. GEOSCIENCES[Internet]. 2012;21(82):173-180. Available from: https://sid.ir/paper/32519/en

    IEEE: Copy

    R. ARFANIA, “ANALYSIS OF THE MESOSCOPIC BRITTLE AND DUCTILE-BRITTLE STRUCTURES IN THE METAMORPHIC AREA OF SOUTHEASTERN EGHLID,” GEOSCIENCES, vol. 21, no. 82, pp. 173–180, 2012, [Online]. Available: https://sid.ir/paper/32519/en

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