Relevant bibliographies by topics / Bassin aquitain offshore

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  2. Dissertations / Theses
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Academic literature on the topic 'Bassin aquitain offshore'

Author: Grafiati
Published: 25 May 2024
Last updated: 31 July 2025

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Journal articles on the topic "Bassin aquitain offshore"

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Torelli, Martina, Isabelle Kowalewski, Veronique Gervais, et al. "Quantification of natural microbial methane from generation to emission in the offshore Aquitaine: A basin modelling approach." Marine and Petroleum Geology 127 (May 2021): 104949. http://dx.doi.org/10.1016/j.marpetgeo.2021.104949.

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Oudet, Julien, Philippe Münch*, Jean Borgomano, et al. "Land and sea study of the northeastern golfe du Lion rifted margin: the Oligocene – Miocene of southern Provence (Nerthe area, SE France)." Bulletin de la Société Géologique de France 181, no. 6 (2010): 591–607. http://dx.doi.org/10.2113/gssgfbull.181.6.591.

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Abstract 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- (p
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de Santana dos Anjos Zerfass, Geise, Dmitry A. Ruban, Farid Chemale Jr., and Henrique Zerfass. "Cenozoic synthem stratigraphic architecture of the SE Brazilian shelf and its global eustatic context: evidence from the Pelotas Basin (offshore Brazil)." Geologos 19, no. 4 (2013): 273–90. http://dx.doi.org/10.2478/logos-2013-0018.

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Abstract The Pelotas Basin, located on the SE Brazilian shelf, has evolved since the Aptian. Stratigraphical data from the basin can be used for delineation of the unconformity-bounded units (synthems) on the shelf, which is a first step towards a full understanding of its stratigraphic architecture, evolution, and hydrocarbon potential. Hiatuses in the Cenozoic succession of the Pelotas Basin are established with both biostratigraphic (planktonic foraminifers and calcareous nannofossils) and isotopic (87Sr/86Sr) data. The seven recognised hiatuses are dated respectively as (1) Palaeocene (Dan
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Fournier, François, Aurélie Tassy, Isabelle Thinon, et al. "Pre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France)." Bulletin de la Société Géologique de France 187, no. 4-5 (2016): 187–215. http://dx.doi.org/10.2113/gssgfbull.187.4-5.187.

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AbstractThe seaward extension of onshore formations and structures were previously almost unknown in Provence. The interpretation of 2D high-resolution marine seismic profiles together with the integration of sea-bottom rock samples provides new insights into the stratigraphic, structural and paleogeographic framework of pre-Messinian Salinity Crisis (MSC) deposits of the Provence continental shelf. Seven post-Jurassic seismic units have been identified on seismic profiles, mapped throughout the offshore Provence area and correlated with the onshore series. The studied marine surface and sub-s
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SOWERBUTTS, ALISON. "Sedimentation and volcanism linked to multiphase rifting in an Oligo-Miocene intra-arc basin, Anglona, Sardinia." Geological Magazine 137, no. 4 (2000): 395–418. http://dx.doi.org/10.1017/s0016756800004246.

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Three extensional phases can be recognized in the northern, Anglona area of the Oligo-Miocene Sardinian Rift during a fifteen million year period which spanned Corsica–Sardinia continental microplate separation and Western Mediterranean back-arc basin opening. In response to this multiphase rifting, a complex facies architecture involving clastic, carbonate and volcanic rocks developed. Integrated onshore facies and structural analysis, dating and offshore seismic data are here used to reconstruct the tectono-stratigraphic history of the Anglona area. Initial late Oligocene extension created a
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Abdulsamad, Esam O., Saleh A. Emhanna, Ramzi S. Fergani, et al. "Miocene Rocks Around the Marádah Oasis, Central Sirt Basin, Libya: Facies Development and Implication on Stratigraphy." Earth Science Research 10, no. 1 (2021): 8. http://dx.doi.org/10.5539/esr.v10n1p8.

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The Miocene rocks of the Marádah Formation have been stratigraphically investigated from four stratigraphical sections around the Marádah Oasis in the Central Sirt Basin of Libya. The field investigations led to the identification of two members, the lower Qarat Jahannam Member and the upper Ar Ráhlah Member. Fourteen sedimentary facies at the outcrop-scale representing a gradual development of sedimentation from a continental clastic witness in the southwestern outcrops to transitional estuarine, lagoonal, and beaches to the proximal offshore in the northern o
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Fillon, Charlotte, Frédéric Mouthereau, Sylvain Calassou, et al. "Post-orogenic exhumation in the western Pyrenees: evidence for extension driven by pre-orogenic inheritance." Journal of the Geological Society, November 23, 2020, jgs2020–079. http://dx.doi.org/10.1144/jgs2020-079.

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We discuss the drivers of the Pyrenean post-orogenic exhumation, including drainage migration, flexural rebound and tectonic reactivation.We provide new low-temperature thermochronological data and inverse thermal modeling from both the hinterland and foreland of the western Pyrenees. Our new thermochronological ages range from 6.6 to 61.4 Ma and reveal a Late Miocene exhumation phase in several massifs. The contrasting thermal histories define a domain of focused exhumation in the western Pyrenees that coincides with the present-day extensional tectonics in a region to the north of the Axial
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Dissertations / Theses on the topic "Bassin aquitain offshore"

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Torelli, Martina. "Modelling Microbial Methane Processes in Marine Environments : from Source to Seep. Insights from Basin Analysis." Electronic Thesis or Diss., Sorbonne université, 2021. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2021SORUS270.pdf.

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Les sédiments marins des marges continentales sont enrichis en Matière Organique Sédimentaire (MOS) qui peut être transformée en méthane par l'activité microbienne. Les précédents résultats obtenus dans le cadre du projet de recherche PAMELA ont permis d'identifier plusieurs points d’émissions de méthane biogénique sur le plateau continental du Golfe de Gascogne et le long des marges du Mozambique et de Madagascar. Afin de mieux comprendre l'impact de la nature de la Matière Organique (MO) sur ces systèmes fluides, nous avons (1) caractérisé la MO et (2) proposé une nouvelle approche de modéli
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Reports on the topic "Bassin aquitain offshore"

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Williams, G. L. Palynological analysis of Aquitaine et al. Hekja 0-71, Saglek Basin, Davis Strait, offshore eastern Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/224259.

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