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<title lang=en>Fast switch from extensional exhumation to thrusting of the Ronda Peridotites (South Spain)</title>
<creator>Frasca, Gianluca</creator>
<creator>Gueydan, Frédéric</creator>
<creator>Poujol, Marc</creator>
<creator>Brun,, Jean-Pierre</creator>
<creator>Parat, Fleurice</creator>
<creator>Monié, Patrick</creator>
<creator>Pichat, Alexandre</creator>
<creator>Mazier, Sophie</creator>
<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>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)</contributor>
<description>International audience</description>
<source>ISSN: 0954-4879</source>
<source>EISSN: 1365-3121</source>
<source>Terra Nova</source>
<publisher>Wiley-Blackwell</publisher>
<identifier>insu-01441962</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01441962</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01441962/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01441962/file/Frasca-TerraNova-2017.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01441962</source>
<source>Terra Nova, Wiley-Blackwell, 2017, 29 (2), pp.117-126. 〈10.1111/ter.12255〉</source>
<identifier>DOI : 10.1111/ter.12255</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12255</relation>
<language>en</language>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Alboran Domain, situated at the western end of the Mediterranean subductionsystem, is characterized by the Ronda Peridotites, one of the world largest exposures of subcontinental mantle. Using U-Pb (LA-ICP-MS) and Ar-Ar dating, we precisely dated twotectonic events associated with the Tertiary exhumation of the Ronda Peridotites. First,shearing along the Crust-Mantle Extensional Shear Zone caused, at ca. 22.5 Ma, mantleexhumation, local partial melting in the deep crust and coeval cooling in the upper crust.Second, the Ronda Peridotites Thrust triggered the final crustal emplacement of theperidotites onto the continental crust at ca. 21 Ma, as testified by granitic intrusions in thethrust hanging-wall. The tectonic evolution of the western Alboran Domain is thereforecharacterized by a fast switch from a continental lithosphere extension in a backarc setting,with sub-continental mantle exhumation, to a rift inversion by thrusting driven by shorteningof the subduction upper plate</description>
<date>2017</date>
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