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<datestamp>2018-01-12</datestamp>
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<title lang=en>La Désirade island (Guadeloupe, French West Indies): a key target for deciphering the role of reactivated tectonic structures in Lesser Antilles arc building,</title>
<creator>Lardeaux, J-Marc</creator>
<creator>Munch, Philippe</creator>
<creator>Corsini, M.</creator>
<creator>Cornee, Jean-Jacques</creator>
<creator>Vérati, Ch.</creator>
<creator>Lebrun, Jean-frederic</creator>
<creator>Quillévéré, F.</creator>
<creator>Melinte-Dobrinescu, M.</creator>
<creator>Léticée, J.-Len</creator>
<creator>Fietzke, J.</creator>
<creator>Mazabraud, Y.</creator>
<creator>Cordey, F.</creator>
<creator>Randrianasolo, A.</creator>
<contributor>Géoazur (GEOAZUR) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - 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>Dynamique de la Lithosphere ; 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) - 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>Bassins ; 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) - 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>Université des Antilles et de la Guyane (UAG)</contributor>
<contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Claude Bernard Lyon 1 (UCBL) - École normale supérieure - Lyon (ENS Lyon)</contributor>
<contributor>GeoEcoMar, Bucarest ; Université du Québec</contributor>
<contributor>Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR)</contributor>
<description>International audience</description>
<source>EISSN: 1777-5817</source>
<source>Bulletin de la Société Géologique de France</source>
<publisher>Société géologique de France</publisher>
<identifier>hal-00830329</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00830329</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00830329</source>
<source>Bulletin de la Société Géologique de France, Société géologique de France, 2013, 184 (1-2), pp.21-34. 〈10.2113/gssgfbull.184.1-2.21〉</source>
<identifier>DOI : 10.2113/gssgfbull.184.1-2.21</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.2113/gssgfbull.184.1-2.21</relation>
<language>en</language>
<subject lang=en>La Désirade island</subject>
<subject lang=en>Lesser Antilles arc</subject>
<subject lang=en>Reactivated tectonic structures</subject>
<subject lang=en>Lower Cretaceous compression</subject>
<subject lang=en>Pliocene to early Pleistocene extension</subject>
<subject lang=en>Active deformation</subject>
<subject lang=en>Vertical displacements</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 this paper we present and discuss new investigations performed on both the magmatic basement and the sedimentary formations of La Désirade. We report structural and sedimentary evidences for several episodes of deformation and displacement occurring prior to the present day tectonics. The main faults, respectively N130 ± 10°, N040 ± 10° and N090 ± 10°, previously considered as marker of the current tectonic regime corresponds to reactivated tectonic structures developed first during late Cretaceous compression and second during Pliocene to early Pleistocene extension. We demonstrate also the importance of late Pliocene-early Pleistocene and middle-late Pleistocene vertical movements in this part of the Lesser Antilles fore-arc as well as the role of compressive tectonics in the over thickened character of the arc basement in the Guadeloupe archipelago</description>
<date>2013-02</date>
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