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Tectonics 28 (2009) TC5002
New tectonic configuration in NE Iran: Active strike-slip faulting between the Kopeh Dagh and Binalud mountains
Esmaeil Shabanian 1, Olivier Bellier 1, Lionel Siame 1, Nicolas Arnaud 2, Mohammad R. Abbassi 3, Jean-Jacques Cocheme
(2009)

In this paper, a combined approach of geomorphic analyses, detailed geological mapping on SPOT 5 satellite images and field surveys, complemented by radiometric dating (Ar-40/Ar-39) allows proposing a new and consistent tectonic configuration for the northeastern Arabia-Eurasia collision zone. It favors a simple strike-slip faulting mechanism in NE Iran accommodating the northward motion of central Iran with respect to Eurasia between the Binalud and Kopeh Dagh mountains. Our results demonstrate that similar to 2 mm/a (similar to 25%) of this northward motion has been transferred from the Binalud to the Kopeh Dagh through the Meshkan Transfer Zone since similar to 5 Ma. The modern state of stress deduced from fault kinematics analyses shows N30 degrees E trending maximum stress axis and confirms a dominant strike-slip faulting mechanism. Combining our geological data with other available data, we conclude that kinematics of deformation can be appropriately described by rigid block faulting in NE Iran; instead, the continuous deformation as it has been thought during the last 3 decades.
1 :  Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE)
CNRS : UMR6635 – Institut de recherche pour le développement [IRD] – INSU – Université de Provence - Aix-Marseille I – Université Paul Cézanne - Aix-Marseille III
2 :  Géosciences Montpellier (GM)
CNRS : UMR5243 – Université Montpellier II - Sciences et techniques
3 :  International Institute of Earthquake Engineering and Seismology, Tehran
inconnue
Planète et Univers/Sciences de la Terre/Géochimie

Sciences de l'environnement/Milieux et Changements globaux
Kopeh Dagh – strike-slip faulting – morphotectonics