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<title lang=en>Aegean tectonics: Strain localisation, slab tearing and trench retreat</title>
<creator>Jolivet, Laurent</creator>
<creator>Faccenna, Claudio</creator>
<creator>Huet, Benjamin</creator>
<creator>Labrousse, Loic</creator>
<creator>Le Pourhiet, Laetitia</creator>
<creator>Lacombe, Olivier</creator>
<creator>Lecomte, Emmanuel</creator>
<creator>Burov, Evgenii, </creator>
<creator>Denèle, Yoann</creator>
<creator>Brun,, Jean-Pierre</creator>
<creator>Gueydan, Frédéric</creator>
<creator>Philippon, Mélody</creator>
<creator>Paul, Anne</creator>
<creator>Salaün, Gwenaëlle</creator>
<creator>Karabulut, Hayrullah</creator>
<creator>Piromallo, Claudia</creator>
<creator>Monié, Patrick</creator>
<creator>Okay, Aral I.</creator>
<creator>Oberhänsli, Roland</creator>
<creator>Pourteau, Amaury</creator>
<creator>Augier, Romain</creator>
<creator>Gadenne, Leslie</creator>
<creator>Driussi, Olivier</creator>
<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>Università “Roma TRE”, Dipartimento Scienze Geologiche, Roma ; Université du Québec</contributor>
<contributor>Department for Geodynamics and Sedimentology ; University of Vienna [Vienna]</contributor>
<contributor>Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géosciences Environnement Toulouse (GET) ; Institut de Recherche pour le Développement (IRD) - Université Paul Sabatier - Toulouse 3 (UPS) - Observatoire Midi-Pyrénées (OMP) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Systèmes Tectoniques ; Géosciences Rennes (GR) ; Université de Rennes 1 (UR1) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire des Sciences de l'Univers de Rennes (OSUR) - Centre National de la Recherche Scientifique (CNRS) - Université de Rennes 1 (UR1) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire des Sciences de l'Univers de Rennes (OSUR) - 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>Kandilli Observatory and Earthquake Research Institute ; Bogazici University [Istanbul]</contributor>
<contributor>INGV, Rome ; Université du Québec</contributor>
<contributor>Avrasya Yerbilimleri Enstitüsü, Istanbul Teknik Universitesi ; Istanbul Teknik Universitesi</contributor>
<contributor>Institut für Erd‐ und Umweltwissenschaften ; Universität Potsdam</contributor>
<description>International audience</description>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>insu-00715950</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00715950</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00715950/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00715950/file/Jolivet-Aegean_Tectonophysics-2012.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00715950</source>
<source>Tectonophysics, Elsevier, 2013, 597-598, pp.1-33. 〈10.1016/j.tecto.2012.06.011〉</source>
<identifier>DOI : 10.1016/j.tecto.2012.06.011</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2012.06.011</relation>
<language>en</language>
<subject lang=en>backarc extension</subject>
<subject lang=en>slab retreat</subject>
<subject lang=en>asthenospheric flow</subject>
<subject lang=en>strain localisation</subject>
<subject lang=en>Aegean Sea</subject>
<subject lang=en>metamorphic core complex</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>We review the geodynamic evolution of the Aegea-Anatolia region and discuss strain localisation there over geological times. From Late Eocene to Present, crustal deformation in the Aegean backarc has localised progressively during slab retreat. Extension started with the formation of the Rhodope Metamorphic Core Complex (Eocene) and migrated to the Cyclades and the northern Menderes massif (Oligocene and Miocene), accommodated by crustal-scale detachments and a first series of core complexes (MCCs). Extension then localised in Western Turkey, the Corinth Rift and the external Hellenic arc after Messinian times, while the North Anatolian Fault penetrated the Aegean Sea. Through time the direction and style of extension have not changed significantly except in terms of localisation. The contributions of progressive slab retreat and tearing, basal drag, extrusion tectonics and tectonic inheritance are discussed and we favour a model (1) where slab retreat is the main driving engine, (2) successive slab tearing episodes are the main causes of this stepwise strain localisation and (3) the inherited heterogeneity of the crust is a major factor for localising detachments. The continental crust has an inherited strong heterogeneity and crustal-scale contacts such as major thrust planes act as weak zones or as zones of contrast of resistance and viscosity that can localise later deformation. The dynamics of slabs at depth and the asthenospheric flow due to slab retreat also have influence strain localisation in the upper plate. Successive slab ruptures from the Middle Miocene to the Late Miocene have isolated a narrow stripe of lithosphere, still attached to the African lithosphere below Crete. The formation of the North Anatolian Fault is partly a consequence of this evolution. The extrusion of Anatolia and the Aegean extension are partly driven from below (asthenospheric flow) and from above (extrusion of a lid of rigid crust).</description>
<date>2013</date>
</dc>
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