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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMULDER, Thierry
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGONTHIER, Eliane
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLECROART, Pascal
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorHANQUIEZ, Vincent
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARCHES, Elodie
dc.contributor.authorVOISSET, M.
dc.date.accessioned2024-11-14T11:23:30Z
dc.date.available2024-11-14T11:23:30Z
dc.date.issued2009-05-01
dc.identifier.issn0264-8172en_US
dc.identifier.urihttps://www.researchgate.net/publication/229372104_Sediment_failures_and_flows_in_the_Gulf_of_Cadiz_eastern_Atlantic
dc.identifier.urioai:researchgate.net:229372104
dc.identifier.urioai:crossref.org:10.1016/j.marpetgeo.2008.02.009
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/203261
dc.description.abstractEnSeveral types of sediment failures in the Gulf of Cadiz were observed using multibeam bathymetry, acoustic imagery and high-resolution seismic. These instabilities are mainly sediment failures and flows. Their width and length vary from 1 to more than 10 km. The failures are mainly related to high sedimentation rates, particularly in places where the Mediterranean Outflow Water (MOW) spills over, such as channel bends and the outer side of the giant contourite levee. Steep slopes are also a trigger for failure at the continental shelf-slope transition, on valley sides, on canyon flanks, and on the sides of bathymetric highs. Other mass movements are related to fluid escape (mud volcanoes) and earthquakes. In areas where the MOW flows along the seafloor, the constant shearing and related erosion can add to the overall stresses. The frequency of failures can be estimated using the deposits resulting of their distal transformations into turbidites.
dc.language.isoENen_US
dc.sourceresearchgate
dc.sourcecrossref
dc.subject.enContour currents
dc.subject.enGulf of Cadiz
dc.subject.enMass wasting
dc.subject.enMediterranean outflow water
dc.subject.enSeafloor instability
dc.subject.enSediment flow
dc.subject.enSlope failure
dc.title.enSediment failures and flows in the Gulf of Cadiz (eastern Atlantic)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.marpetgeo.2008.02.009en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalMarine and Petroleum Geologyen_US
bordeaux.page660-672en_US
bordeaux.volume26en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue5en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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