Zobrazeno 1 - 10
of 68
pro vyhledávání: '"Jean-Claude Faugères"'
Autor:
Eliane Gonthier, Pierre Cirac, Jean-Claude Faugeres, Michel Cremer, Jean-François Bourillet, Mathieu Gaudina
Publikováno v:
Scientia Marina, Vol 70, Iss S1, Pp 89-100 (2006)
Acoustic and core data have recently been collected on the shelf break and the upper part of the slope of the south Aquitaine continental margin. They reveal the major role played by mass-flow gravity processes in deposit erosion and redistribution,
Externí odkaz:
https://doaj.org/article/96bc806243d7462eb114a12779b9e8cb
Publikováno v:
Sedimentology. 58:571-577
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Columbia Channel (CCS) system is a depositional system located in the South Brazilian Basin, south of the Vitoria–Trindade volcanic chain. It lies in a WNW–ESE direction on the continental rise and abyssal plain, at a depth of between 4200 an
Publikováno v:
Sedimentology. 56:997-1015
Hummocky cross-stratification is a sedimentary structure which is widely interpreted as the sedimentary record of an oscillatory current generated by energetic storm waves remobilizing surface sediment on the continental shelf. Sedimentary structures
Publikováno v:
Comptes Rendus Geoscience. 341:36-48
High resolution seismic data display four channel sets in front of the Lake of Hourton and the Lake of Lacanau covering a faulted and folded unit (U2) deposited during a high sea level at the end of the Burdigalian. The next unit (U3-1) shows sigmoid
Publikováno v:
Marine Geology. 236:223-245
Very few sediment records allow addressing the paleoceanographic changes that took place on orbital and/or sub-Milankovitch time scales in the South–West Atlantic. Here, a set of sediment cores located across a deep channel-levee system in the Sout
Autor:
Mathieu Gaudina, Eliane Gonthier, Pierre Cirac, Jean-François Bourillet, Jean-Claude Faugères, Michel Cremer
Publikováno v:
Scientia Marina, Vol 70, Iss S1, Pp 89-100 (2006)
Scientia Marina; Vol. 70 No. S1 (2006); 89-100
Scientia Marina; Vol. 70 Núm. S1 (2006); 89-100
Scientia Marina
Consejo Superior de Investigaciones Científicas (CSIC)
Scientia Marina; Vol. 70 No. S1 (2006); 89-100
Scientia Marina; Vol. 70 Núm. S1 (2006); 89-100
Scientia Marina
Consejo Superior de Investigaciones Científicas (CSIC)
Acoustic and core data have recently been collected on the shelf break and the upper part of the slope of the south Aquitaine continental margin. They reveal the major role played by mass-flow gravity processes in deposit erosion and redistribution,
Autor:
Francisco Javier Hernandéz-Molina, L. M. Fernandez, Ferran Estrada, Thierry Mulder, Y. Fuchey, E. Habgood, Dominique Poirier, F. Lobo Sanchez, P. Freitas, Antje H L Voelker, Neil H. Kenyon, Vincent Hanquiez, J. Morel, Pascal Lecroart, E. Le Drezen, Jean-Claude Faugères, E. Llave-Barranco, Christian Gorini, M. Voisset, Eliane Gonthier
Publikováno v:
Geo-Marine Letters. 23:7-18
Recent multibeam bathymetry and acoustic imagery data provide a new understanding of the sedimentary system located in the Gulf of Cadiz which is under the influence of a strong current, the Mediterranean Outflow Water (MOW). When it comes out from t
Autor:
Andrea G.P.R. Figueiredo, Jean-Claude Faugères, Eliane Gonthier, Adriano R. Viana, Pierre Anschutz
Publikováno v:
Marine Geology. 199:159-180
This paper is an attempt to show how one may discriminate turbiditic and contouritic processes in the deposition of deep-sea accumulations. The case study is the Sao Tome deep-sea ‘channel levee’ system in the South Brazilian Basin. This system i
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, Elsevier, 2003, 20 (6-8), pp.861-882. ⟨10.1016/j.marpetgeo.2003.01.003⟩
Marine and Petroleum Geology, 2003, 20 (6-8), pp.861-882. ⟨10.1016/j.marpetgeo.2003.01.003⟩
Marine and Petroleum Geology, Elsevier, 2003, 20 (6-8), pp.861-882. ⟨10.1016/j.marpetgeo.2003.01.003⟩
Marine and Petroleum Geology, 2003, 20 (6-8), pp.861-882. ⟨10.1016/j.marpetgeo.2003.01.003⟩
Hyperpycnal flows form in the marine environment when river discharge enters the ocean with suspended concentrations in excess of 36 kg m 23 due to buoyancy considerations, or as little as 1- 5 kg m 23 when convective instability is considered. They