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dc.rights.licenseopenen_US
hal.structure.identifierTOTAL S.A.
dc.contributor.authorBUSSON, Jean
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorTELES, Vanessa
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMULDER, Thierry
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorJOSEPH, Philippe
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorGUY, Nicolas
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorBOUZIAT, Antoine
hal.structure.identifierCentre scientifique et Technique Jean Feger [CSTJF]
hal.structure.identifierEnvironnement Méditerranéen et Modélisation des Agro-Hydrosystèmes [EMMAH]
dc.contributor.authorDANQUIGNY, Charles
hal.structure.identifierCentre scientifique et Technique Jean Feger [CSTJF]
dc.contributor.authorPOLI, Emmanuelle
hal.structure.identifierCentre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE]
hal.structure.identifierInstitut Pythéas [OSU PYTHEAS]
hal.structure.identifierInstitut de Recherche pour le Développement [IRD]
dc.contributor.authorBORGOMANO, Jean
dc.date.accessioned2024-02-05T10:42:16Z
dc.date.available2024-02-05T10:42:16Z
dc.date.issued2021-02
dc.identifier.issn1612-510Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187798
dc.description.abstractEnSlope failure and landslides are widespread on the submarine slopes of carbonate platforms. They represent a key component of their stratigraphic evolution and a major geohazard. Several Quaternary slope failures and mass transport complexes were identified on the western slope and margin of the Great Bahama Bank (GBB) platform. This study evaluates several hypotheses for the preconditions associated to these events, in relation with the stratigraphic and environmental history of the platform. The forward stratigraphic simulator Dionisos Flow™ allows the slope stratigraphic evolution to be reconstructed on a 2D platform-to-basin section at high temporal resolution according to the eustatic and environmental history of the last 1.7 Myr. The hydromechanical simulator A2 is applied on this high-resolution stratigraphic grid for computing the mechanical stratigraphy of the section, that is the spatiotemporal pore pressure and stress state distribution. The simulated precondition of the platform margin during glacial lowstands results from the combination of two factors: transient overpressure generation by lateral fluid flow from the emerged platform and the steepening stratigraphic trend of the platform. No significant pore fluid overpressure is generated under high sedimentation rates or as a result of shift in hydrostatic gradient during sea-level falls. Precondition in the lower slope is not achieved in this 2D simulation, with the horizontal stress distribution counteracting the effect of overpressure build-up. It is found that cemented levels in the lower slope succession do not represent a significant preconditioning factor.
dc.language.isoENen_US
dc.subject.enSubmarine landslides
dc.subject.enCarbonate slope
dc.subject.enPore fluid overpressure
dc.subject.enFailure precondition
dc.subject.enForward modelling
dc.subject.enMechanical stratigraphy
dc.subject.enLateral fluid flow
dc.title.enSubmarine landslides on a carbonate platform slope : forward numerical modelling of mechanical stratigraphy and scenarios of failure precondition
dc.typeArticle de revueen_US
dc.identifier.doi10.1007/s10346-020-01510-7en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
bordeaux.journalLandslidesen_US
bordeaux.page595-618en_US
bordeaux.volume18en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03152498
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
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