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The deep-sea Armorican depositional system (Bay of Biscay), a multiple source, ramp model

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.contributor.authorLE SUAVÉ, R.
dc.contributor.authorBOURILLET, J. F.
dc.contributor.authorAUFFRET, G. A.
dc.contributor.authorG., Auffret
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorFAUGERES, Jean Claude
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorPUJOL, Claude
dc.contributor.authorT., Garlan
dc.date.accessioned2024-11-15T13:05:01Z
dc.date.available2024-11-15T13:05:01Z
dc.date.issued2001-01-04
dc.identifier.issn0276-0460en_US
dc.identifier.urihttps://www.researchgate.net/publication/225417260_The_deep-sea_Armorican_depositional_system_Bay_of_Biscay_a_multiple_source_ramp_model
dc.identifier.urioai:researchgate.net:225417260
dc.identifier.urioai:crossref.org:10.1007/s003670100061
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/203309
dc.description.abstractEnThe deep-sea Armorican depositional system, located in the central part of the Bay of Biscay, is a medium-sized turbidite system with a surface area of more than 30,000 km2. The whole system is a mud/sand-rich submarine ramp on a passive margin. The medial ramp is characterised by the presence of six distinct tributary channels which form three systems: the Guilcher, Crozon and Cornouaille systems. The distal ramp corresponds to divergent braided secondary channels and associated lobes. Variations in hydrodynamic conditions on the outer Armorican Shelf during the last climatic cycle are the major factor controlling facies shifts and system growth. Thus, the Armorican depositional system is a delta-fed submarine ramp during low sea-level glacial conditions, and an outer shelf-fed submarine ramp at times of sea-level rise.
dc.language.isoENen_US
dc.sourceresearchgate
dc.sourcecrossref
dc.title.enThe deep-sea Armorican depositional system (Bay of Biscay), a multiple source, ramp model
dc.typeArticle de revueen_US
dc.identifier.doi10.1007/s003670100061en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeo-Marine Lettersen_US
bordeaux.page219-232en_US
bordeaux.volume20en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue4en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04785449
hal.version1
hal.date.transferred2024-11-15T13:05:03Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geo-Marine%20Letters&rft.date=2001-01-04&rft.volume=20&rft.issue=4&rft.spage=219-232&rft.epage=219-232&rft.eissn=0276-0460&rft.issn=0276-0460&rft.au=ZARAGOSI,%20Sebastien&LE%20SUAV%C3%89,%20R.&BOURILLET,%20J.%20F.&AUFFRET,%20G.%20A.&G.,%20Auffret&rft.genre=article


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