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Understanding continent-ocean sediment transfer ArchiMer
Mulder, Thierry; Cirac, Pierre; Gaudin, Mathieu; Bourillet, Jean-francois; Trainer, J.; Normand, Alain; Weber, O.; Griboulard, R.; Jouanneau, Jean-marie; Anschutz, Pierre; Jorissen, Frans.
Submarine canyons are narrow but deep submarine valleys that extend for hundreds of meters. They represent the most impressive structures that shape the present morphology of passive continental margins. They can occur off the mouth of rivers: the Tagus, Zaire, Amazon, and Orinoco in the Atlantic; the Indus in the Indian Ocean; and the Var, Rhone, and Ebro in the Mediterranean. Some are at times disconnected from any stream mouth such as the Nazare canyon, off Portugal, despite the fact that it is close to the coast. Some were connected to a river mouth during lowstands of sea level, such as the Wilmington canyon in the northwest Atlantic, or the Blackmud canyon in the northeast Atlantic.
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Ano: 2004 URL: http://archimer.ifremer.fr/doc/00071/18201/15769.pdf
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Sedimentary processes and facies on the northern Aquitaine shelf, France. ArchiMer
Cirac, Pierre; Berne, Serge; Castaing, Patrice; Weber, Olivier.
The Aquitaine shelf in France is a storm-dominated shelf similar to the Californian shelf in the US. It exhibits a thin veneer (about 1-2 m) of sandy sediments overlying coarse-grained deposits. This surficial sand sheet is shaped into various bed forms corresponding to the contrasted physical processes operating at different water depths and time-scales. These bed forms are: a) sand patches separated by depressions or 'furrows', b) large transverse dunes and c) large wave ripples. The overall architecture of the sand cover is considered as resulting from the stacking of several storm beds. During the last post-glacial sea-level rise, the magnitude of reworking processes progressively decreased as a result of increasing water depth. This is demonstrated by...
Tipo: Text Palavras-chave: Northern Aquitaine shelf Sequence deposits Bedforms Hydrodynamic processes Sedimentology Plate forme nord aquitaine Séquences de dépôt Formes sédimentaires; Processus hydrodynamiques Sédimentologie.
Ano: 2000 URL: https://archimer.ifremer.fr/doc/2000/publication-526.pdf
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