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<title lang=en>Land and sea study of the northeastern golfe du Lion rifted margin: the Oligocene – Miocene of southern Provence (Nerthe area, SE France)</title>
<creator>Oudet, J.</creator>
<creator>Munch, Philippe</creator>
<creator>Borgomano, J.</creator>
<creator>Quillévéré, F.</creator>
<creator>Melinte-Dobrinescu, M.</creator>
<creator>Demory, François</creator>
<creator>Viseur, Sophie</creator>
<creator>Cornee, Jean-Jacques</creator>
<contributor>Geologie des Systèmes et des Reservoirs Carbonates (GSRC - EA 4234) ; Université de Provence - Aix-Marseille 1</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>Laboratoire de Géologie des Systèmes et Réservoirs Carbonatés EA 4229 ; Université de Provence - Aix-Marseille 1</contributor>
<contributor>Paléoenvironnement et paléobiosphère (PP) ; Université Claude Bernard Lyon 1 (UCBL) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>National Institute of Geology and Marine Geoecology ; National Institute of Geology and Marine Geoecology</contributor>
<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>Géologie des systémes et des réservoirs carbonatés - EA4234 (GSRC) ; Université de Provence - Aix-Marseille 1 - Centre National de la Recherche Scientifique (CNRS)</contributor>
<source>EISSN: 1777-5817</source>
<source>Bulletin de la Société Géologique de France</source>
<publisher>Société géologique de France</publisher>
<identifier>hal-00558497</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00558497</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00558497</source>
<source>Bulletin de la Société Géologique de France, Société géologique de France, 2010, 181 (6), pp.591-608. 〈10.2113/gssgfbull.181.6.591〉</source>
<identifier>DOI : 10.2113/gssgfbull.181.6.591</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.2113/gssgfbull.181.6.591</relation>
<language>en</language>
<subject lang=it>Oligocene</subject>
<subject lang=it>Miocene</subject>
<subject lang=it>Mediterranean</subject>
<subject lang=it>Golfe du Lion</subject>
<subject lang=it>Bio-magnetostratigraphy</subject>
<subject lang=it>Land and sea approach</subject>
<subject>[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>In the western Mediterranean Sea, the Liguro-Provençal Basin (LPB) is a key area for studying passive margins because of its recent formation and abundance of onshore and offshore data. The Nerthe area located in the northern margin of LPB provides the unique continuous Oligo-Miocene deposits contemporaneous of the transition rifting to drifting. However, the age of the deposits remains debated and the link between outcrops and offshore seismic data is poorly constrained. The purpose of this paper is double. First, we intend to propose a new chronostratigraphic frame based on bio- (planktonic foraminifera, calcareous nannofossils) and magneto-stratigraphy. Second, we aim to make, through the integration of new highly time-resolved seismic data and field works, a coherent onshore-offshore link concretized by a 3D geological model. The new temporal and spatial data presented in this paper allow correlating the Oligo-Miocene sequences, defining their geometry and specifying precisely the timing of syn- and post-rift stages. The first marine transgression is now precisely dated latest Chattian within the syn-rift deposits and appears to be synchronous with the first marine deposits in the offshore wells and other marginal basins. The transition from syn-rift to post-rift appears to last 3.3 Ma at maximum, between 21.8 and 18.5 Ma (late Aquitanian to early Burdigalian). It is underlined by two major erosional unconformities bearing a hiatus of around 1 Ma. The post-rift started with a major marine transgression that is now dated from middle Burdigalian, at around 18.5 Ma, as elsewhere in the LPB. Contrarily to recent proposals, the post-rift deposits are widely represented on the northeastern margin of the "Golfe du Lion". There, the subsidence of the margin was low during the syn-rift and the transitional periods and high during the post-rift. The onset of this high post-rift subsidence appears to be synchronous with the slowdown of the Corsica-Sardinia block (CSb) motion.</description>
<date>2010-11-01</date>
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