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<title lang=en>New tectonic configuration in NE Iran: Active strike-slip faulting between the Kopeh Dagh and Binalud mountains</title>
<creator>Shabanian, Esmaeil</creator>
<creator>Bellier, Olivier</creator>
<creator>Siame, Lionel</creator>
<creator>Arnaud, Nicolas</creator>
<creator>Abbassi, Mohammad R.</creator>
<creator>Cocheme, Jean-Jacques</creator>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>International Institute of Earthquake Engineering and Seismology, Tehran ; Université du Québec</contributor>
<description>International audience</description>
<source>ISSN: 0278-7407</source>
<source>Tectonics</source>
<publisher>American Geophysical Union (AGU)</publisher>
<identifier>hal-00420909</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00420909</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00420909</source>
<source>Tectonics, American Geophysical Union (AGU), 2009, 28, pp.TC5002. 〈10.1029/2008TC002444〉</source>
<identifier>DOI : 10.1029/2008TC002444</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2008TC002444</relation>
<language>en</language>
<subject lang=en>Kopeh Dagh</subject>
<subject lang=en>strike-slip faulting</subject>
<subject lang=en>morphotectonics</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>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.</description>
<date>2009</date>
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