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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:35:32Z</responseDate> <request identifier=oai:HAL:insu-00816463v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:insu-00816463v1</identifier> <datestamp>2018-01-12</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:UPMC</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:BRGM</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GEOAZUR</setSpec> <setSpec>collection:OCA</setSpec> <setSpec>collection:ENS-LYON</setSpec> <setSpec>collection:LGL-TPE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:UNIV-BREST</setSpec> <setSpec>collection:UNICE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:UNIV-AMU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> <setSpec>collection:LGO</setSpec> <setSpec>collection:CMM</setSpec> <setSpec>collection:UCA-TEST</setSpec> <setSpec>collection:UNIV-COTEDAZUR</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Pliocene to Pleistocene carbonate systems of the Guadeloupe archipelago, French Lesser Antilles: a land and sea study (the KaShallow project)</title> <creator>Munch, Philippe</creator> <creator>Lebrun, Jean-Frédéric</creator> <creator>Cornee, Jean-Jacques</creator> <creator>Thinon, Isabelle</creator> <creator>Guennoc, Pol</creator> <creator>Marcaillou, Boris</creator> <creator>Begot, Jacques</creator> <creator>Bertrand, Guillaume</creator> <creator>Bès De Berc, Séverine</creator> <creator>Biscarrat, Kevin</creator> <creator>Claud, Clarisse</creator> <creator>De Min, Lyvane</creator> <creator>Fournier, François</creator> <creator>Gailler, Lydie</creator> <creator>Graindorge, David</creator> <creator>Léticée, Jean-Len</creator> <creator>Marie, Lionel</creator> <creator>Mazabraud, Yves</creator> <creator>Melinte-Dobrinescu, Mihaela Carmen</creator> <creator>Moissette, Pierre</creator> <creator>Quillévéré, Frédéric</creator> <creator>Verati, Chrystèle</creator> <creator>Randrianasolo, Auran</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>Géologie des systèmes carbonatés (EA 4234) ; Université de Provence - Aix-Marseille 1</contributor> <contributor>Université des Antilles et de la Guyane (UAG)</contributor> <contributor>Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)</contributor> <contributor>Institut de Recherche pour le Développement (IRD [Nouvelle-Calédonie])</contributor> <contributor>Domaines Océaniques (LDO) ; Centre National de la Recherche Scientifique (CNRS) - Institut d'écologie et environnement - Observatoire des Sciences de l'Univers - Université de Brest (UBO) - Institut national des sciences de l'Univers (INSU - CNRS)</contributor> <contributor>National Institite of Marine Geology & Geoecology ; GEOECOMAR</contributor> <contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; École normale supérieure - Lyon (ENS Lyon) - Université Claude Bernard Lyon 1 (UCBL) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor> <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>DyETI - INSU CNRS EFRD Projects</contributor> <description>International audience</description> <source>Bulletin Société Géologique de France</source> <identifier>insu-00816463</identifier> <identifier>https://hal-insu.archives-ouvertes.fr/insu-00816463</identifier> <source>https://hal-insu.archives-ouvertes.fr/insu-00816463</source> <source>Bulletin Société Géologique de France, 2013, 184 (1-2), pp.99-110. 〈10.2113/gssgfbull.184.1-2.99〉</source> <identifier>DOI : 10.2113/gssgfbull.184.1-2.99</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.2113/gssgfbull.184.1-2.99</relation> <language>en</language> <subject lang=en>Lesser Antilles fore-arc</subject> <subject lang=en>Guadeloupe</subject> <subject lang=en>Carbonate platforms</subject> <subject lang=en>Pliocene</subject> <subject lang=en>Pleistocene</subject> <subject lang=en>Vertical motion</subject> <subject lang=en>Land and sea study</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>This work presents a synthesis of the present-day knowledge on both emerged and submerged carbonate platforms of the Guadeloupe archipelago. Onshore and offshore data acquired during the KaShallow project are presented. Since the early Zanclean, some isolated platforms developed onto a Jurassic to Tortonian basement which displayed reliefs inherited from a major extensional tectonic episode dated from −8 to −5 Ma. Marie-Galante, Grande Terre and the southern shelf of Grande-Terre show strong similarities with Zanclean to Gelasian red-algal facies upward changing into early Calabrian coral facies. A major erosional unconformity (SB2) was recognized and allows to distinguish two early Calabrian formations (Calcaires à Agaricia Formation and Calcaires à Acropora Formation). The final emersion of these platforms is late Calabrian. The La Désirade platform displays Zanclean to early Piacenzian red-algal facies upward changing into coral facies. This platform emerged as soon as in the late Piacenzian. The island subsided again in relation with later extensional tectonic episode and early Calabrian reef platform then unconformably deposited. The Colombie bank deposits comprise Pliocene basinal deposits overlain by late Calabrian coral reefs. The Flandre bank might have emerged synchronously with La Désirade but was drowned only in the late Pleistocene-Holocene interval. Four extensional tectonic episodes have been identified in the late Miocene-Recent interval. Their effects depend on the location of the platforms within the fore-arc.</description> <date>2013-01-31</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>