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Role of the Kazerun fault system in active deformation of the Zagros fold-and-thrust belt (Iran)
Authors:Christine Authemayou  Olivier Bellier  Dominique Chardon  Zaman Malekzade  Mohammad Abassi
Institution:1. Centre européen de recherche et d''enseignement de géosciences de l''environnement (UMR CNRS 6635), université Aix–Marseille-3, BP 80, 13545 Aix-en-Provence cedex 4, France;2. International Institute of Earthquake Engineering and Seismology, Sholeh str., 8th Kohestan, Pasdaran, Tehran, I.R. Iran
Abstract:Field structural and SPOT image analyses document the kinematic framework enhancing transfer of strike-slip partitioned motion from along the backstop to the interior of the Zagros fold-and-thrust belt in a context of plate convergence slight obliquity. Transfer occurs by slip on the north-trending right-lateral Kazerun Fault System (KFS) that connects to the Main Recent Fault, a major northwest-trending dextral fault partitioning oblique convergence at the rear of the belt. The KFS formed by three fault zones ended by bent orogen-parallel thrusts allows slip from along the Main Recent Fault to become distributed by transfer to longitudinal thrusts and folds. To cite this article: C. Authemayou et al., C. R. Geoscience 337 (2005).
Keywords:Zagros  Strike-slip faulting  Tectonics  Fault kinematics  Oblique convergence  Partitioning  Segmentation  Zagros  Faille décrochante  Tectonique  Cinématique de failles  Convergence oblique  Partitionnement  Segmentation
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