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Статті в журналах з теми "Marges continentales – Andes (nord)"
Regnauld, Hervé, and Yves-F. Thomas. "Les pentes continentales des marges passives. Le cas de l'Atlantique du Nord-Est (The continental slopes of passive margins. The case of the NE Atlantic)." Bulletin de l'Association de géographes français 68, no. 2 (1991): 117–31. http://dx.doi.org/10.3406/bagf.1991.1566.
Повний текст джерелаChew, David M., and Cees R. Van Staal. "The Ocean – Continent Transition Zones Along the Appalachian – Caledonian Margin of Laurentia: Examples of Large-Scale Hyperextension During the Opening of the Iapetus Ocean." Geoscience Canada 41, no. 2 (May 7, 2014): 165. http://dx.doi.org/10.12789/geocanj.2014.41.040.
Повний текст джерелаOliveros, Veronica, Pablo Moreno-Yaeger, and Laura Flores. "Igneous Rock Associations 25. Pre-Pliocene Andean Magmatism in Chile." Geoscience Canada, July 10, 2020, 65–82. http://dx.doi.org/10.12789/geocanj.2020.47.158.
Повний текст джерелаДисертації з теми "Marges continentales – Andes (nord)"
Aizprua, Carlos. "Structure et développement du bassin d'avant-arc du sud-ouest des Andes du Nord." Electronic Thesis or Diss., Université de Lille (2018-2021), 2021. http://www.theses.fr/2021LILUR001.
Повний текст джерелаThe SW Ecuador‐NW Peru forearc region is the southernmost location, where the Caribbean large igneous province (CLIP) interacted with the South American margin since the Late Cretaceous. The accretion of the CLIP to the margin led to the entrapment of the North Andean crustal Sliver, conforming the underlying basement of the forearc region in Ecuador, whereas in NW Peru, forearc depocenters involve rocks of continental affinity. Many existing tectonic reconstructions have treated these two areas independently, largely based on their crustal affinities. In contrast, this study integrates previous studies into an analysis of unpublished seismic profiles, potential field data, outcrop stratigraphy, and recent studies dealing with the dynamics of allochthonous terrane accretion along continental margins. Our integrated approach shows that SW Ecuador was dominated by a Late Cretaceous deforming outer wedge, which may have constituted a remnant of a northeast or northwest dipping obliquely obducted oceanic block at the edge of the CLIP. This tectonic phase was governed by plate instability, affecting NW Peru and SW Ecuador, followed by reestablishment of the margin by early Eocene. The resulting margin configuration and the spatial distribution of the different tectonic elements seem to have played a key role in the further Cenozoic development of the forearc region. The model presented in this study proposes that the accretion of buoyant oceanic terranes may have had a profound impact on the early margin configuration of SW Ecuador and NW Peru and led to the development of localized but genetically related forearc depocenters
Soler, Pierre. "Contribution à l'étude du magmatisme associé aux marges actives : pétrographie, géochimie et géochimie isotopique du magmatisme crétacé à pliocène le long d'une transversale des Andes du Pérou central : implications géodynamiques." Paris 6, 1991. http://www.theses.fr/1991PA066637.
Повний текст джерелаPoydenot, Frédéric. "Le canyon de Toulon : morphologie et sédimentation (Méditerranée nord-occidentale)." Aix-Marseille 2, 1993. http://www.theses.fr/1993AIX22095.
Повний текст джерелаLapouyade, Agnès. "Quantification, variabilité saisonnière et comparaison du transport advectif de la matière particulaire sur différentes marges continentales en Méditerranée nord." Aix-Marseille 3, 2001. http://www.theses.fr/2001AIX30110.
Повний текст джерелаThe continental margins are the receptacle of the continental inputs and form a buffer zone with the open ocean. Significant quantities of matter and energy transit on these margins under the effect of a very active hydrodynamism. This work focus on the study of advective transport between the continental shelf and the open ocean, of the paniculate matter and organic carbon. The objectives are to provide a seasonal and, if possible, annual quantification of advective paniculate flux and to consider the importance of the shelf-basin exchanges in the total budgets of the margins by identification of the principal mechanisms responsible for these exchanges and their relative importance. Three sites in the Northern Mediterranean were studied within the framework of the european programs METRO-MED and MATER: Gulf of Lions, Gulf of Thermaikos and the shelf of Samothrace. Data of eight oceanographic cruises were used. They cover, at least, the two principal hydrological seasons: the stratified summer period and the not stratified winter period Concentrations of paniculate organic carbon and matter are derived from light-transmission data and water sample analyses. The circulation is determined from the geostrophic current field. The uncertainty on the transport estimation, related to the error on the prediction of the particle concentrations and to the error on speeds, is assessed. Particulate matter flux result mainly from the water flux variations rather than from variations of paniculate matter concentration. These fluxes vary seasonally and present a maximum intensity in winter. Also the autochthonous and allochtonous paniculate inputs as well as the intensity of the exchange processes between the shelf and the basin, on these three margins present a winter intensification. The studied margins show different behaviours with regard to the exchanges from paniculate matter and organic carbon with the open ocean. A compilation of annual budgets estimated from the seasonal budgets of the margins in the Northern Mediterranean, suggest that the Gulf of Lions exports paniculate matter offshore whereas the other margins import matter
Pascal, André. "Les Systèmes biosédimentaires urgoniens Aptien-Albien sur la marge Nord-ibérique /." Dijon : Institut des sciences de la terre, 1985. http://catalogue.bnf.fr/ark:/12148/cb34840930j.
Повний текст джерелаThommeret, Michel. "Tectonique comparee des marges continentales sarde (mer tyrrhenienne-italie) et falicienne (nord-ouest de l'iberie)." Paris 6, 1990. http://www.theses.fr/1990PA066701.
Повний текст джерелаMitouard, Pierre. "La marge active nord-péruvienne : étude paléomagnétique et modélisation analogique." Paris 11, 1991. http://www.theses.fr/1991PA112164.
Повний текст джерелаLe, Breton Eline. "L'ouverture différentielle de l'océan Atlantique Nord-Est et ses effets sur les déformations postbreak-up des marges continentales." Phd thesis, Université Rennes 1, 2012. http://tel.archives-ouvertes.fr/tel-00714418.
Повний текст джерелаPincivy, Alix. "Géochronologie 40Ar/39Ar et analyse structurale de la zone Humber des Appalaches de Gaspésie (Québec, Canada) : implications sur la tectonique des Appalaches du nord." Rennes 1, 2003. http://www.theses.fr/2003REN10017.
Повний текст джерелаBaltzer, Agnès. "Dynamique sédimentaire des marges de nouvelle Ecosse et des entreés de la Manche au quaternaire." Brest, 1994. http://www.theses.fr/1994BRES2027.
Повний текст джерелаЧастини книг з теми "Marges continentales – Andes (nord)"
TUGEND, Julie, and Isabelle THINON. "L’ouverture du golfe de Gascogne à la limite de plaque ibéro-européenne." In Évolution des Pyrénées au cours du cycle varisque et du cycle alpin 1, 253–87. ISTE Group, 2023. http://dx.doi.org/10.51926/iste.9124.ch6.
Повний текст джерела