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Title

steady state deformation in the shear zones of the Sanandaj-Sirjan metamorphic belt, Neyriz region

Pages

  97-108

Abstract

 Kinematic and structural studies on the deformed rocks of the Sanandaj-Sirjan Metamorphic Belt as a part of the Zagros Orogeny show that the Deformation was occurred under greenschist-to amphibolite-facies conditions. A dominant top-to-the-SE sense of shear is confirmed by asymmetric boudins, mica fish, mantled porphyroclasts, drag folds, asymmetric crenulation cleavage and quartz c-axis fabrics. The mean Kinematic Vorticity Number analyses based on the quartz fabrics and rotated porphyroclasts revealed relative contribution of ~44% pure shear and ~56% simple shear components during ductile general shear Deformation associated with a transpressional flow regime. The variable quantities of simple shear relative to time reveals that the earlier phases of Deformation developed during a pure shear-dominated regime whereas the later stages took place in a simple shear-dominated regime.

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    APA: Copy

    Keshavar, Saeede, FAGHIH, ALI, SHAHPASANDZADEH, MAJID, & ZAREI, SAEED. (2018). steady state deformation in the shear zones of the Sanandaj-Sirjan metamorphic belt, Neyriz region. TECTONICS, 2(5 ), 97-108. SID. https://sid.ir/paper/267886/en

    Vancouver: Copy

    Keshavar Saeede, FAGHIH ALI, SHAHPASANDZADEH MAJID, ZAREI SAEED. steady state deformation in the shear zones of the Sanandaj-Sirjan metamorphic belt, Neyriz region. TECTONICS[Internet]. 2018;2(5 ):97-108. Available from: https://sid.ir/paper/267886/en

    IEEE: Copy

    Saeede Keshavar, ALI FAGHIH, MAJID SHAHPASANDZADEH, and SAEED ZAREI, “steady state deformation in the shear zones of the Sanandaj-Sirjan metamorphic belt, Neyriz region,” TECTONICS, vol. 2, no. 5 , pp. 97–108, 2018, [Online]. Available: https://sid.ir/paper/267886/en

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