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<datestamp>2018-01-13</datestamp>
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<title lang=en>Miocene crustal extension following thrust tectonic in the Lower Sebtides units (internal Rif, Ceuta Peninsula, Spain): Implication for the geodynamic evolution of the Alboran domain</title>
<creator>Homonnay, Emmanuelle</creator>
<creator>Corsini, Michel</creator>
<creator>Lardeaux, Jean-Marc</creator>
<creator>Romagny, Adrien</creator>
<creator>Munch, Philippe</creator>
<creator>Bosch, Delphine</creator>
<creator>CENKI-TOK, Benedicte</creator>
<creator>Ouazzani-Touhami, Mohamed</creator>
<contributor>Géoazur (GEOAZUR) ; Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) ; Bureau de Recherches Géologiques et Minières (BRGM) (BRGM) - Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géodynamique - UMR7327 ; Bureau de Recherches Géologiques et Minières (BRGM) (BRGM) - Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) ; Bureau de Recherches Géologiques et Minières (BRGM) (BRGM) - Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - 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>Département de Géologie Université de Abdelmalek Esaadi ; Université de Abdelmalek Esaadi</contributor>
<description>International audience</description>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>insu-01682810</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01682810</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01682810</source>
<source>Tectonophysics, Elsevier, 2018, 722, pp.507 - 535. 〈10.1016/j.tecto.2017.11.028〉</source>
<identifier>DOI : 10.1016/j.tecto.2017.11.028</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2017.11.028</relation>
<language>en</language>
<subject lang=en>Rif belt</subject>
<subject lang=en> Gibraltar arc</subject>
<subject lang=en> Metamorphism</subject>
<subject lang=en> Geochronology</subject>
<subject lang=en> Orogenic wedge</subject>
<subject lang=en> Back-arc extension</subject>
<subject>[SDU] Sciences of the Universe [physics]</subject>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>In Western Mediterranean, the Rif belt in Morocco is part of the Gibraltar Arc built during the Tertiary in the framework of Eurasia-Africa convergence. The structural and metamorphic evolution of the internal units of this belt as well as their timing, crucial to constrain the geodynamic evolution of the Alboran Sea, is still largely debated.Our study on the Ceuta Peninsula (Northern Rif) provides new structural, petrological and geochronological data (U-Th-Pb, Ar-Ar), which allow to precise the tectono-metamorphic evolution of the Lower Sebtides metamorphic units with:(1) a syn-metamorphic thrusting event developed under granulite facies conditions (7–10 kbar and 780–820 °C). A major thrust zone, the Ceuta Shear Zone, drove the emplacement of metapelites and peridotitic lenses from the Ceuta Upper Unit over the orthogneisses of the Monte Hacho Lower Unit. This compressional event ended during the Upper Oligocene.(2) an extensional event developed at the boundary between amphibolite and greenschist facies conditions (400–550 °C and 1–3 kbar). During this event, the Ceuta Shear Zone has been reactivated as a normal fault. Normal ductile shear zones contributed to the final exhumation of the metamorphic units during the Early Miocene.We propose that the compressional event is related to the formation of an orogenic wedge located in the upper plate, in a backward position, of the subduction zone driving the geodynamic evolution of the Alboran domain. In this context, the episode of lithospheric thinning could be related to the opening of the Alboran basin in a back-arc position.Furthermore, unlike the previous models proposed for the Rif belt, the tectonic coupling between mantle peridotites and crustal metamorphic rocks occurred in Ceuta Peninsula at a depth of 20–30 km under high temperature conditions, before the extensional event, and thus cannot be related to the back-arc extension.</description>
<date>2018-01</date>
<contributor>European Project : 612572, EC:FP7:PEOPLE, FP7-PEOPLE-2013-IRSES, MEDYNA(2014)</contributor>
<relation>info:eu-repo/grantAgreement/EC/FP7/612572/EU/MAGHREB-EU RESEARCH STAFF EXCHANGE ON GEODYNAMICS, GEOHZARDS, AND APPLIED GEOLOGY IN NORTH-WEST AFRICA/MEDYNA</relation>
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