untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T18:30:39Z</responseDate>
<request identifier=oai:HAL:insu-01009592v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:insu-01009592v1</identifier>
<datestamp>2018-01-12</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:UNIV-BREST</setSpec>
<setSpec>collection:BRGM</setSpec>
<setSpec>collection:UPMC</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-AMU</setSpec>
<setSpec>collection:IFREMER</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:OCA</setSpec>
<setSpec>collection:GEOAZUR</setSpec>
<setSpec>collection:ISTEP</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:UNICE</setSpec>
<setSpec>collection:CEREGE</setSpec>
<setSpec>collection:OSU-INSTITUT-PYTHEAS</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:PSL</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:CDF</setSpec>
<setSpec>collection:ISTEP-EMBS</setSpec>
<setSpec>collection:IRD</setSpec>
<setSpec>collection:UPMC_POLE_3</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>Discovery of Messinian canyons and new seismic stratigraphic model, offshore Provence (SE France): Implications for the hydrographic network reconstruction</title>
<creator>Tassy, Aurélie</creator>
<creator>Fournier, F.</creator>
<creator>Munch, Philippe</creator>
<creator>Borgomano, J.</creator>
<creator>Thinon, Isabelle</creator>
<creator>Fabri, Marie-Claire</creator>
<creator>Rabineau, Marina</creator>
<creator>Arfib, B.</creator>
<creator>Begot, Jacques</creator>
<creator>Beslier, Marie-Odile</creator>
<creator>Cornee, Jean-Jacques</creator>
<creator>Fournillon, Arnaud</creator>
<creator>Gorini, Christian</creator>
<creator>Guennoc, Pol</creator>
<creator>Leonide, P.</creator>
<creator>Oudet, J.</creator>
<creator>Paquet, Fabien</creator>
<creator>Sage, Françoise</creator>
<creator>TOULLEC, R.</creator>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</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 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>TOTAL S.A. ; TOTAL FINA ELF</contributor>
<contributor>Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)</contributor>
<contributor>Laboratoire Environnmement LER/PAC ; Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)</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>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>
<description>International audience</description>
<source>ISSN: 0264-8172</source>
<source>Marine and Petroleum Geology</source>
<publisher>Elsevier</publisher>
<identifier>insu-01009592</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01009592</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01009592/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01009592/file/Mar-Pet-Tassy.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01009592</source>
<source>Marine and Petroleum Geology, Elsevier, 2014, 57, pp.25-50. 〈10.1016/j.marpetgeo.2014.05.001〉</source>
<identifier>DOI : 10.1016/j.marpetgeo.2014.05.001</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marpetgeo.2014.05.001</relation>
<language>en</language>
<subject lang=en>Western Mediterranean</subject>
<subject lang=en>Provence continental shelf</subject>
<subject lang=en>Base Plio-Quaternary surface</subject>
<subject lang=en>Submarine canyon</subject>
<subject lang=en>Karst</subject>
<subject lang=en>Offshore seismic data</subject>
<subject lang=en>Shallow coring</subject>
<subject lang=en>Geological mapping</subject>
<subject>[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy</subject>
<subject>[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The interpretation of high-resolution 2D marine seismic profiles together with the analysis of sea-bottom cores allowed a stratigraphic and structural framework of the Provence continental shelf to be proposed. The integration of onshore and offshore stratigraphy, structure and geomorphology provided new insights into Messinian paleotopography and paleohydrography. A geological map of the offshore Provence continental shelf, isobath map of the base Plio-Quaternary surface are presented for the first time in this area. The base Plio-Quaternary surface is a polyphased unconformity that is composed of deep canyons developed by fluvial erosion during the Messinian event, and wave-cut surfaces formed during post-Messinian transgressions. The study evidenced a deep, E-W-trending canyon (Bandol canyon) connected to the head of the Cassidaigne canyon, and filled with up to 600 m-thick Plio-Quaternary deposits. The development of canyons on the Provence margin during the Messinian event was dominantly controlled by the lithology and structure of pre-Messinian formations. A map of the Messinian paleo-drainage network is proposed to explain the presence of deep canyons in the Eastern area and the lack of incision in the Western area. An underground karst drainage scheme is proposed, linked with the current submarine Port-Miou spring.</description>
<date>2014-11-03</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
