untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T18:24:00Z</responseDate>
<request identifier=oai:HAL:hal-01306672v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-01306672v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:MNHN</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:LGL-TPE</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:IPH-ACTU</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:IPH</setSpec>
<setSpec>collection:ENS-LYON</setSpec>
<setSpec>collection:UNIV-PERP</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>The Messinian erosional surface and early Pliocene reflooding in the Alboran Sea: New insights from the Boudinar basin, Morocco</title>
<creator>CORNEE, Jean-jacques</creator>
<creator>MUNCH, Philippe</creator>
<creator>ACHALHI, Mohammed</creator>
<creator>MERZERAUD, Gilles</creator>
<creator>Azdimousa, Ali</creator>
<creator>Quillévéré, F.</creator>
<creator>Melinte-Dobrinescu, M.</creator>
<creator>Chaix, Christian</creator>
<creator>Ben moussa, Abdelkhalak</creator>
<creator>LOFI, Johanna</creator>
<creator>SERANNE, Michel</creator>
<creator>Moisette, Pierre</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>Geologie des Reservoirs et Ressources ; 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>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>Université Mohamed 1er, faculté des sciences, Oujda</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>Histoire naturelle de l'Homme préhistorique (HNHP) ; Muséum National d'Histoire Naturelle (MNHN) - Université de Perpignan Via Domitia (UPVD) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Université Abdelmalek Esaadi, Tetuán</contributor>
<contributor>Transferts en milieux poreux ; 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>
<description>International audience</description>
<source>ISSN: 0037-0738</source>
<source>Sedimentary Geology</source>
<publisher>Elsevier</publisher>
<identifier>hal-01306672</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01306672</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01306672</source>
<source>Sedimentary Geology, Elsevier, 2016, 333, pp.115-129. 〈10.1016/j.sedgeo.2015.12.014〉</source>
<identifier>DOI : 10.1016/j.sedgeo.2015.12.014</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.sedgeo.2015.12.014</relation>
<language>en</language>
<subject lang=en>Alboran Sea</subject>
<subject lang=en>Morocco</subject>
<subject lang=en>Boudinar basin</subject>
<subject lang=en>Messinian Salinity Crisis</subject>
<subject lang=en>Zanclean flooding</subject>
<subject>[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>New investigations in the Neogene Boudinar basin (Morocco) provide new information about the Messinian Salinity Crisis (MSC) and Zanclean reflooding in the southern part of the Alboran realm (westernmost Mediterranean). Based on a new field, sedimentological and palaeontological analyses, the age and the geometry of both the Messinian erosional surface (MES) and the overlying deposits have been determined. The MES is of late Messinian age and was emplaced in subaerial settings. In the Boudinar basin, a maximum of 200 m of Miocene sediments was eroded, including late Messinian gypsum blocks. The original geometry of the MES is preserved only when it is overlain by late Messinian continental deposits, conglomeratic alluvial fans or lacustrine marly sediments. These sediments are interpreted as indicators of the sea-level fall during the MSC. Elsewhere in the basin, the contact between late Messinian and early Pliocene deposits is a low-angle dipping, smooth surface that corresponds to the early Pliocene transgression surface that subsequently re-shaped the regressive MES. The early Pliocene deposits are characterized by: (i) their onlap onto either the basement of the Rif chain or the late Miocene deposits; (ii) lagoonal deposits at the base to offshore marls and sands at the top (earliest Pliocene; 5.33–5.04 Ma interval; foraminifer zone PL1); (iii) marine recovery occurring in the 5.32–5.26 Ma interval; and (iv) the change from lagoonal to offshore environments occurring within deposits tens of metres thick. This information indicates that at least the end of the reflooding period was progressive, not catastrophic as previously thought.</description>
<date>2016-03-15</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
