The French Atlantic margin and deep-sea submarine systems
dc.rights.license | open | en_US |
dc.contributor.author | BOURILLET, Jean-Francois | |
hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
dc.contributor.author | ZARAGOSI, Sebastien
IDREF: 189039159 | |
hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
dc.contributor.author | MULDER, Thierry | |
dc.date.accessioned | 2024-11-14T13:23:03Z | |
dc.date.available | 2024-11-14T13:23:03Z | |
dc.date.issued | 2006-10-28 | |
dc.identifier.issn | 0276-0460 | en_US |
dc.identifier.uri | http://archimer.ifremer.fr/doc/2006/publication-2137.pdf | |
dc.identifier.uri | ftarchimer:oai:archimer.ifremer.fr:2137 | |
dc.identifier.uri | oai:researchgate.net:29491327 | |
dc.identifier.uri | oai:crossref.org:10.1007/s00367-006-0042-2 | |
dc.identifier.uri | https://oskar-bordeaux.fr/handle/20.500.12278/203271 | |
dc.description.abstractEn | The sedimentary infill of the Bay of Biscay off Ireland, UK, France and Spain took place in four phases. The last one (35 Ma to present) is characterised by gravitational, pelagic, contouritic and glacigenic processes leading to the setup of three deep sea systems. To the North, the Celtic and Armorican fans are fed by a "canyon-dominated" margin and its connection with the "Manche" palaeoriver, which drained a large area of western Europe. To the South, the Cap-Ferret fan results from the evolution of a "tectonic-dominated" margin and the erosion of the Pyrenee mountains. | |
dc.language.iso | EN | en_US |
dc.source | base | |
dc.source | researchgate | |
dc.source | crossref | |
dc.title.en | The French Atlantic margin and deep-sea submarine systems | |
dc.type | Article de revue | en_US |
dc.identifier.doi | 10.1007/s00367-006-0042-2 | en_US |
dc.subject.hal | Sciences de l'environnement | en_US |
bordeaux.journal | Geo-Marine Letters | en_US |
bordeaux.page | 311-315 | en_US |
bordeaux.volume | 26 | en_US |
bordeaux.hal.laboratories | EPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805 | en_US |
bordeaux.issue | 6 | en_US |
bordeaux.institution | Université de Bordeaux | en_US |
bordeaux.institution | CNRS | en_US |
bordeaux.peerReviewed | oui | en_US |
bordeaux.inpress | non | en_US |
bordeaux.import.source | dissemin | |
hal.identifier | hal-04783009 | |
hal.version | 1 | |
hal.date.transferred | 2024-11-14T13:23:05Z | |
hal.popular | non | en_US |
hal.audience | Internationale | en_US |
hal.export | true | |
workflow.import.source | dissemin | |
dc.rights.cc | Pas de Licence CC | en_US |
bordeaux.COinS | ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geo-Marine%20Letters&rft.date=2006-10-28&rft.volume=26&rft.issue=6&rft.spage=311-315&rft.epage=311-315&rft.eissn=0276-0460&rft.issn=0276-0460&rft.au=BOURILLET,%20Jean-Francois&ZARAGOSI,%20Sebastien&MULDER,%20Thierry&rft.genre=article |
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