Literatura académica sobre el tema "Remplissage sédimentaire"
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Artículos de revistas sobre el tema "Remplissage sédimentaire":
Campy, Michel. "Étude sédimentologique du remplissage". Gallia préhistoire. Suppléments 27, n.º 1 (1989): 27–48. http://dx.doi.org/10.3406/galip.1989.2552.
Visset, Lionel y Didier Voeltzel. "Le confluent Erdre-Loire, étude pollenanalytique du remplissage sédimentaire atlantique (Nantes-France)." Bulletin de l'Association française pour l'étude du quaternaire 26, n.º 3 (1989): 121–27. http://dx.doi.org/10.3406/quate.1989.1900.
Braillard, L. "Remplissages quaternaires et paléohydrologie des vallées sèches d’Ajoie (Jura tabulaire, Suisse)". Geographica Helvetica 64, n.º 3 (30 de septiembre de 2009): 148–56. http://dx.doi.org/10.5194/gh-64-148-2009.
Benssaou, M. y Naïma Hamoumi. "L'Anti-Atlas occidental du Maroc : remplissage sédimentaire d'un bassin de type rift intracontinental au Cambrien inférieur". Géologie Méditerranéenne 26, n.º 3 (1999): 259–79. http://dx.doi.org/10.3406/geolm.1999.1661.
Vergnolle, Christine. "Géométrie du remplissage sédimentaire des bassins de Sarria et Monforte ( Galice, Espagne ) et évolution géomorphologique régionale". Mélanges de la Casa de Velázquez 21, n.º 1 (1985): 331–46. http://dx.doi.org/10.3406/casa.1985.2449.
Mokeddem, Zohra, Agnès Baltzer, Martine Clet-Pellerin, Anne Véronique Walter-Simonnet, Richard Bates, Yvon Balut y Chantal Bonnot-Courtois. "Fluctuations climatiques enregistrées depuis 20 000ans dans le remplissage sédimentaire du loch Sunart (Nord-Ouest de l’Écosse)". Comptes Rendus Geoscience 339, n.º 2 (febrero de 2007): 150–60. http://dx.doi.org/10.1016/j.crte.2006.11.004.
Peiry, J. L. y J. P. Bravard. "Evolution naturelle d'un remplissage sédimentaire intramontagnard et impacts des aménagements contemporains : L'exemple de la vallée de l'Arve (74)". La Houille Blanche, n.º 3-4 (junio de 1989): 221–25. http://dx.doi.org/10.1051/lhb/1989018.
Chairi, Raja. "Etude du remplissage sédimentaire d’un système hypersalin de la Tunisie orientale au cours du Quaternaire récent : la sebkha de Moknine". Quaternaire, n.º 16/2 (1 de agosto de 2005): 107–17. http://dx.doi.org/10.4000/quaternaire.328.
Niftah, Sabah, André Debénath y Jean-Claude Miskovsky. "Origine du remplissage sédimentaire des grottes de Témara (Maroc) d’après l’étude des minéraux lourds et l’étude exoscopique des grains de quartz". Quaternaire, n.º 16/2 (1 de agosto de 2005): 73–83. http://dx.doi.org/10.4000/quaternaire.295.
Yamba, T. K. y A. Boven. "Evolution Pliocène et Quaternaire du remplissage sédimentaire dans le sud du bassin du lac Edouard, branche occidentale du Rift Est-Africain". Journal of African Earth Sciences 26, n.º 3 (abril de 1998): 423–39. http://dx.doi.org/10.1016/s0899-5362(98)00024-4.
Tesis sobre el tema "Remplissage sédimentaire":
Gourronc, Marine. "Morphologie et remplissage sédimentaire des vallées martiennes : marqueurs des conditions climatiques pré-amazoniennes". Nantes, 2015. http://www.theses.fr/2015NANT2006.
Nowadays Mars has a cold and dry climate. At some locations its surface is more than 3. 5 Gy old and exhibits valleys, channels, terraces and deltas attesting the occurrence of liquid water in the past. This fluid is currently unstable on the surface of the planet, suggesting these morphologies would involve different climatic conditions from the current ones. What did early Martian climate look like? lt is one of the main issues regarding this planet. Among the geomorphological evidence classically used to reconstruct past climates, Martian valleys are numerous and heterogeneously distributed thus particularly attractive to study. Their morphologies can inform on the climatic conditions prevailing at the time of their formation and/or later during their evolution. The objective of this thesis is to contribute to solve the enigma concerning Martian pre-Amazonian (> 3. 5 Gy) climatic conditions by focusing on the study of equatorial valleys and the equatorial canyon of Valles Marineris. Our study reveals that the morphometry and spatial organization of some Martian valleys differ significantly from those of common terrestrial fluvial and sapping valleys. By contrast, they share a lot of similarities with terrestrial subglacial tunnel valleys. The subglacial or pro- glacial melting of surface ice deposits is plausible as an origin of some Martian valleys under cold climatic conditions. Moreover, regional geomorphological reconstitutions of Valles Marineris reveal that this valley system had witnessed glacial processes since its formation. Current glacial relicts of this former filling, probably several billion years old, still subsist protected under a debris cover. This study suggests the possibility that pre-Amazonian atmospheric conditions on Mars do not require to be significantly different from the current ones
Neurdin-Trescartes, Jacqueline. "Le remplissage sédimentaire du bassin néogène du Chélif, modèle de référence de bassins intramontagneux". Pau, 1992. http://www.theses.fr/1992PAUU3021.
Salles, Tristan. "Modélisation numérique du remplissage sédimentaire des canyons et chenaux sous-marins par approche génétique". Bordeaux 1, 2006. http://www.theses.fr/2006BOR13254.
Alzaga, Ruiz Humberto. "Architecture et remplissage sédimentaire du bassin profond du Golfe du Mexique : modélisation stratigraphique et structurale du transect de Tuxpan". Montpellier 2, 2008. http://www.theses.fr/2008MON20230.
The Deep Basin of the Gulf of Mexico (DBGM) is localized to the east of Mexico, to the southeast United states and to the west of the ocean Atlantic. The interest zone principal of this study on the part deep of the Gulf of Mexico has a bathymetries that varies of 200 to 3750 m, and understands continental slope and the abyssal plain. The geodynamic evolutions the Deep Basin of the Gulf of Mexico (DBGM) begins to the Triassic Jurassic with the rupture and the opening of a continental rift, in the sector south of the American North Tectonic Plate. This opening has the relative movement towards the southeast of the Yucatan Block, this will be the origin of the DBGM (Tectonics Analysis et al. , 2002). This geodynamic of continental rift is followed by a step of post-rift and spreading center. The basins continental margin developed to the west of the Gulf of Mexico, while oceanic crust formed in the DBGM. The basins of the passive margin then evolved under the effect the a thermal subsidence. The thermal subsidence of the margin next was perturbed by the orogeny Laramide, that restructured the architecture stratigraphic with silicoclastic deposits between the elements morphotectonic following: the tectonic front of the Sierra Madre Oriental (SMO), the foreland basin Chicontepec, the Tuxpan Platform (Golden Lane), the continental slope and the abyssal plain, these two last provinces morphotectonic belonging to the DBGM. During the Early Paleogene, the effects of the thermal subsidence of the passive margin were stressed by the tectonic load of the orogeny Laramide (SMO), allowing thus the development of a foreland basin flexural. In this framework geodynamic, the principal sedimentary transfers carried out themselves tectonic front "SMO" towards the DBGM. The principal source of sediments clastic is linked to the erosion of the chain of mountains "SMO". During the Paleocene and the Early Eocene, the architecture of the sediments silico-clastic syn-tectonic deposited in submarine fans are characterized by sliding, turbidities A and B of Bouma Facies and levee channels. After the end of the flexural subsidence, the thermal subsidence of the passive margin continued during the Late Eocene, the Oligocene and the Neogene, allowing the development of a new sedimentary prisms progradant. The sedimentary fillings up again are constituted levee-channels, sand bars platform and delta systems. During the Neogene a roll-over system developed on the slope of the DBGM, this roll-over detachment at a surface of clays of the Eocene-Oligocene. This system has more than 60% of the sediments silicoclastique of the Miocene. This sedimentary deposit go to of river-delta features towards sliding gravities associated to slump facies
Manalt, Frédéric. "Enregistrement lacustre de la dernière déglaciation dans les Alpes nord-occidentales : Le remplissage sédimentaire du lac d'Annecy (Haute-Savoie)". Chambéry, 1998. https://tel.archives-ouvertes.fr/tel-00715689.
Quiquerez, Amélie. "Le remplissage des bassins sédimentaires carbonatés : contraintes géologiques et modélisations numériques". Université Joseph Fourier (Grenoble), 1999. http://www.theses.fr/1999GRE10269.
HUSSON, Eglantine. "Interaction géodynamique/karstification et modélisation géologique 3D des massifs carbonatés : Implication sur la distribution prévisionnelle de la karstification. Exemple des paléokarts crétacés à néogènes du Languedoc montpelliérain". Phd thesis, Université Montpellier II - Sciences et Techniques du Languedoc, 2013. http://tel.archives-ouvertes.fr/tel-00936257.
Carcaud, Nathalie. "Remplissages des fonds de vallées de la Moselle et de la Meurthe en Lorraine sédimentaire". Nancy 2, 1992. http://www.theses.fr/1992NAN21017.
Chevalier, Michel. "Tectonique récente, effondrements et remplissages sédimentaires cénozoi͏̈ques dans le Domaine du Lac de Grand-Lieu". Nantes, 1987. http://www.theses.fr/1987NANT2008.
Oguadinma, Vivian Onyinyechukwu. "The submarine canyon heads of the Niger delta : structural controls, sedimentary infilling and Cenozoic evolution". Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR087.
Submarine canyons are major corridors for transferring sediments from continents to deep submarine basins. Considered transit structures sealed by distal mud, canyons have little perspective in reservoir geology. The source of the sediments, the timing of inputs, and the transport mechanisms in submarine canyons differ from one margin to another depending on the climatic and geodynamic contexts, making it a vast field of study. This work presents the results of a high-resolution 3D seismic survey of a south-eastern submarine canyon in the Niger Delta, the Galabor Canyon. After a literature review, two articles submitted to BSGF are presented in this dissertation. The first article focuses on seismic geomorphology and the relationships between gravity deformation (shale ridges, detachment faults) and canyon dynamics. The seismic volume studied, wedged at the well (gamma ray and biostratigraphic calibration), was explored through (i) vertical sections along and across the thalwegs of the canyon and (ii) seismic attribute maps of key horizons. The confinement of turbiditic flows in intra slope basin bordered by shale ridges explains much of the trapping of sand at the upper slope. Channel processes are responsible for sorting and concentrating sand in meander belts that extend far beyond the initial incision. The second article concerns sequential stratigraphy. Two 100,000-year-old deposition sequences are identified, separated by a dated horizon of 0.99 Ma. In each sequence, the sand is not sourced by an incised valley but by the regressive submarine erosion of shelf-edge deltas. The sand is bypassed in the falling stage system tract, dominated by mass transport deposits, and preserved in the low stand system tract. The transgressive system tract, which is thick and forms an excellent seal above the sandy reservoir, is dominated by fine hemipelagic sedimentation and the high stand system tract is absent. Questions such as sediment source and flow transformations between gravity and tractive mechanisms remain unanswered
Capítulos de libros sobre el tema "Remplissage sédimentaire":
ARETZ, Markus, Élise NARDIN, Frédéric CHRISTOPHOUL y Julien DENAYER. "Bassins sédimentaires et évolution du relief associés au cycle varisque en France et dans les pays limitrophes". En La chaîne varisque en France 2, 135–215. ISTE Group, 2024. http://dx.doi.org/10.51926/iste.9100.ch3.
Actas de conferencias sobre el tema "Remplissage sédimentaire":
Cherif, E., Rafik Absi, Abdellatif Ouahsine y Philippe Sergent. "Simulations numériques de l’évolution des fonds et effet du mélange turbulent sur le transport sédimentaire : Application au remplissage d’une fosse d’extraction". En Journées Nationales Génie Côtier - Génie Civil. Editions Paralia, 2006. http://dx.doi.org/10.5150/jngcgc.2006.017-c.
Informes sobre el tema "Remplissage sédimentaire":
Logan, C. E., H. A. J. Russell, A. K. Burt, A. Burt, R. P. M. Mulligan, D. R. Sharpe y A. F. Bajc. A three-dimensional surficial geology model of southern Ontario. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/pudw24j7tx.