untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T15:41:47Z</responseDate>
<request identifier=oai:HAL:hal-00407864v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-00407864v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:sde</setSpec>
<setSpec>collection:GEOAZUR</setSpec>
<setSpec>collection:OCA</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:UNIV-TLSE3</setSpec>
<setSpec>collection:OMP-LMTG</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:UPMC</setSpec>
<setSpec>collection:OMP</setSpec>
<setSpec>collection:SDE</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:OMP-GET</setSpec>
<setSpec>collection:UNICE</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:UNIV-AMU</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
<setSpec>collection:UCA-TEST</setSpec>
<setSpec>collection:UNIV-COTEDAZUR</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>Onshore to offshore reconstruction of the Messinian erosion surface in Western Sardinia, Italy: Implications for the Messinian salinity crisis</title>
<creator>Cornee, Jean-Jacques</creator>
<creator>Maillard, A.</creator>
<creator>Conesa, G.</creator>
<creator>Garcia, F.</creator>
<creator>Saint-Martin, J.P.</creator>
<creator>Sage, F.</creator>
<creator>Munch, P.</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>Laboratoire des Mécanismes et Transfert en Géologie (LMTG) ; Université Paul Sabatier - Toulouse 3 (UPS) - Observatoire Midi-Pyrénées (OMP) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Centre de Sédimentologie-Paléontologie (FRE2761) ; Université de Provence - Aix-Marseille 1</contributor>
<contributor>Paléobiodiversité et paléoenvironnements ; Université Pierre et Marie Curie - Paris 6 (UPMC) - 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>
<description>International audience</description>
<source>ISSN: 0037-0738</source>
<source>Sedimentary Geology</source>
<publisher>Elsevier</publisher>
<identifier>hal-00407864</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00407864</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00407864</source>
<source>Sedimentary Geology, Elsevier, 2008, 210 (1-2), pp.48-60. 〈10.1016/j.sedgeo.2008.06.005〉</source>
<identifier>DOI : 10.1016/j.sedgeo.2008.06.005</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.sedgeo.2008.06.005</relation>
<language>en</language>
<subject lang=en>Messinian</subject>
<subject lang=en>Erosion surface</subject>
<subject lang=en>Sardinia</subject>
<subject lang=en>Karst</subject>
<subject lang=en>Mediterranean</subject>
<subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>New outcrops in the Sinis peninsula (Sardinia, Italy) allow a detailed description of the Messinian erosion surface. The correlation between outcrops, industrial seismic data and data collected offshore Oristano from a recent cruise permits reconstruction of the geometry of this surface from presently emerged interfluves to the deep canyons offshore, with: - onshore: an eroded karstic plateau presently cropping out over a 20 km × 5 km area. Well-preserved karst structures occur locally and can form several metres high reliefs. The southernmost edge of the plateau is limited by a cliff. The karstic plateau and the cliff are sealed by transgressive deposits of Pliocene age; - offshore, an interfluve zone with a mostly flat and low-angle dipping plateau, westward dissected by paleovalleys which were identified down to a depth of 2000 m. In the Oristano Gulf, Messinian paleovalleys were also identified. The Capo San Marco paleocliff was probably located on the edge of a canyon. Onshore, only one major erosion surface was identified, located at the top the Messinian sequence. Offshore, this surface extends down to the abyssal plain. The surface was emplaced above deposits related to the Terminal Carbonate Complex. This indicates that the marginal evaporites are older than the major drawdown of the Mediterranean sea-level. The major drawdown is related to the deposition of the deep evaporites.</description>
<date>2008</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
