Littérature scientifique sur le sujet « Marine to continental transition »
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Articles de revues sur le sujet "Marine to continental transition"
Liu, Chao, Hai Tao Xue, Shuang Wang et Yu Jiao Sun. « Study on Law of Structural Evolution and Sedimentary Evolution for North Uskyurt Basin ». Advanced Materials Research 671-674 (mars 2013) : 302–5. http://dx.doi.org/10.4028/www.scientific.net/amr.671-674.302.
Texte intégralBera, M. K., A. Sarkar, P. P. Chakraborty, R. S. Loyal et P. Sanyal. « Marine to continental transition in Himalayan foreland ». Geological Society of America Bulletin 120, no 9-10 (1 septembre 2008) : 1214–32. http://dx.doi.org/10.1130/b26265.1.
Texte intégralSingh, B. P. « Marine to continental transition in Himalayan foreland : Discussion ». Geological Society of America Bulletin 122, no 5-6 (6 avril 2010) : 954–55. http://dx.doi.org/10.1130/b26532.1.
Texte intégralBera, M. K., A. Sarkar, P. P. Chakraborty, R. S. Loyal et P. Sanyal. « Marine to continental transition in Himalayan foreland : Reply ». Geological Society of America Bulletin 122, no 5-6 (6 avril 2010) : 956–59. http://dx.doi.org/10.1130/b26591.1.
Texte intégralWei, Zhifu, Yongli Wang, Gen Wang, Ting Zhang, Wei He, Xueyun Ma et Xiaoli Yu. « Enrichment Mechanism of the Upper Carboniferous-Lower Permian Transitional Shale in the East Margin of the Ordos Basin, China : Evidence from Geochemical Proxies ». Geofluids 2020 (6 novembre 2020) : 1–14. http://dx.doi.org/10.1155/2020/8867140.
Texte intégralCui, Z., S. Davies, K. S. Carslaw et A. M. Blyth. « The response of precipitation to aerosol through riming and melting in deep convective clouds ». Atmospheric Chemistry and Physics Discussions 10, no 11 (25 novembre 2010) : 29007–50. http://dx.doi.org/10.5194/acpd-10-29007-2010.
Texte intégralCui, Z., S. Davies, K. S. Carslaw et A. M. Blyth. « The response of precipitation to aerosol through riming and melting in deep convective clouds ». Atmospheric Chemistry and Physics 11, no 7 (15 avril 2011) : 3495–510. http://dx.doi.org/10.5194/acp-11-3495-2011.
Texte intégralNing, Shitan, Peng Xia, Fang Hao, Jinqiang Tian, Yong Fu et Ke Wang. « Pore Fractal Characteristics between Marine and Marine–Continental Transitional Black Shales : A Case Study of Niutitang Formation and Longtan Formation ». Fractal and Fractional 8, no 5 (13 mai 2024) : 288. http://dx.doi.org/10.3390/fractalfract8050288.
Texte intégralMonesi, Edoardo, Giovanni Muttoni, Giancarlo Scardia, Fabrizio Felletti, Fabio Bona, Benedetto Sala, Fabrizio Tremolada, Carlo Francou et Gianluca Raineri. « Insights on the opening of the Galerian mammal migration pathway from magnetostratigraphy of the Pleistocene marine-continental transition in the Arda River section (northern Italy) ». Quaternary Research 86, no 2 (septembre 2016) : 220–31. http://dx.doi.org/10.1016/j.yqres.2016.07.006.
Texte intégralMourier, Thomas, Peter Bengtson, Michel Bonhomme, Emile Buge, Henri Cappettta, Jean-Yves Crochet, Monique Feist et al. « The Upper Cretaceous - Lower Tertiary marine to continental transition in the Bagua basin, northern Peru - Paleontology, biostratigraphy, radiometry, correlations ». Newsletters on Stratigraphy 19, no 3 (26 octobre 1988) : 143–77. http://dx.doi.org/10.1127/nos/19/1988/143.
Texte intégralThèses sur le sujet "Marine to continental transition"
Alves, Luizemara Soares. « Estudo da margem continental ibérica ocidental com base em dados gravimétricos e magnetométricos regionais ». Universidade do Estado do Rio de Janeiro, 2012. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=6240.
Texte intégralPotential field methods are known as a very useful tool to regional studies. On Western Iberia, gravimetric and magnetometric data could be helpful to understand some questions about the offshore tectonic framework. In this area, both continental break-up features and inherited continental basement structures have a strong contribution to compose the regional geophysical response on gravimetric and magnetometric maps. This work aims to correlate observed geophysical features of the Iberian margin with some geological models about the tectonic framework of Western Iberia, already published on literature. Filtered maps were used to recognize different geophysical signatures, which were computed from both calculated Bouguer gravity and total magnetic field, such as total horizontal gradient, tilt derivative, vertical derivative, and vertical integration. The continental crustal domain was defined from gravity data interpretation using an enhanced total horizontal gradient of Bouguer Anomaly maps. Magnetic data was used to identify three more regional offshore domains that could indicate three types of non-sialic crust. Two of them are proposed as transitional domains. The landward transitional crust has a very weak regional magnetic response, and the seaward one is a high amplitude anomaly domain, similar to oceanic magnetic response. The oceanic crustal boundary was not confirmed, but a third offshore domain, seaward from C34 isochron, could be considered as oceanic crust by its magnetic pattern. Some basement lineaments were indicated in the offshore continental crust. Gravimetric and magnetic features coincide in terms of their direction and position with Variscan suture zones mapped onshore. Therefore these contacts could correspond the offshore continuation of these Paleozoic features, such as the Ossa-Morena Zone and Centro-Ibérica Zone suture zone. In this interpretation, offshore continental crust could be formed by units from Southwest Iberia. It allows considering the Porto-Tomar fault as a part of a swath of strike-slip deformation, where mesozoic basins are located.
Bouton, Anthony. « Facteurs de contrôle extrinsèques des dépôts microbiens récents en domaine de transition continental-marin ». Thesis, Dijon, 2016. http://www.theses.fr/2016DIJOS012/document.
Texte intégralLithified microbial deposits, considered as microbialites, are organosedimentary structures observed since 3.5 billion years. Understanding the mechanisms and environmental conditions leading to their formation may provide valuable information about the origin of life on Earth. Our interest on this research topic has increased owing to the economic implications of these deposits, especially concerning the hydrocarbons. The reconstruction of the environments associated with microbial structures remains uncertain in the fossil record, especially between marine and continental domains. These two contrasting environments were studied through two modern examples: (1) a marine-fed lagoon area in Cayo Coco (Cuba), and the continental lake of the Great Salt Lake (Utah, USA) in order to identify diagnostic criteria allowing to distinguish both environments in the fossil record.Microbialite result from mineralization and lithification of microbial mats under the influence of metabolic chemical reactions (intrinsic) related to the activity of the microbial biomass and environmental (extrinsic) conditions. The objective of this PhD is to replace microbial deposits, at different scales, in their context of formation to highlight the significance of extrinsic parameters on: (1) the mineralization processes and the formation of microbialites, (2) the morphologies of observed microbial structures, (3) their spatial distribution, and (4) the relationship between microbial mats and microbialite and their environment
Nunez, del Prado Hernando. « Systèmes de dépôts et évolution sédimentaire des séries de transition marin-continental dans le synclinorium de Guarga (bassin sud-pyrénéen) : (Province de Huesca N-Espagne) ». Pau, 1986. http://www.theses.fr/1986PAUU300X.
Texte intégralMAGALHÃES, José Ricardo Gonçalves. « Compartimentação tectono-sedimentar da Bacia da Paraíba, a partir da integração de métodos potenciais e interpretação sísmica de dados OFFSHORE ». Universidade Federal de Pernambuco, 2015. https://repositorio.ufpe.br/handle/123456789/17212.
Texte intégralMade available in DSpace on 2016-06-30T17:44:49Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Dissertação_JoséRicardo.pdf: 6453119 bytes, checksum: 0ee0cb3c7c1782b42a982a22935271cb (MD5) Previous issue date: 2015-07-31
PRH-26/ ANP
Vários trabalhos têm tentado abordar a evolução das margens conjugadas do Atlântico, incluindo o nordeste do Brasil e o oeste da África. Entretanto, o avanço de pesquisas anteriores tem sido dificultado em razão da falta de dados na região marginal da porção oriental do nordeste do Brasil, principalmente na área inserida entre a Zona de Cisalhamento de Pernambuco e o Alto de Touros. Este fato tem imposto limitações ao desenvolvimento de modelos regionais sobre a evolução geotectônica e paleogeográfica desta região, assim como na correlação com sua contraparte na África. Nesta dissertação é apresentada uma investigação realizada com base em dados gravimétricos, magnéticos e sísmicos regionais. Os resultados mostraram que esta região representa um alto do embasamento com a orientação regional das principais estruturas tectônicas (ENE-WSW), ortogonais as estruturas desenvolvidas durante o processo de abertura das bacias da Paraíba e da Plataforma de Natal (NNE-SSW e NNW-SSE). Sobre o embasamento continental formou-se uma plataforma estreita com uma cobertura sedimentar pouco espessa (0,8-2,5 km) e uma quebra abrupta da plataforma, criando uma vasta zona de bypass através do talude. A análise de uma seção sísmica profunda revelou que a crosta continental afinada (crosta transicional) representa uma estreita zona e que o limite crosta continental-oceânica (COB) está localizado a aproximadamente 100 km a leste da atual linha de costa, na Bacia da Paraíba, e a 70 km, na Bacia da Plataforma de Natal. A modelagem geofísica, integrada com a interpretação sísmica, indica que esta região é caracterizada por um afinamento abrupto da crosta continental, com a consequente ascensão súbita da Moho. Também há evidências da existência de uma zona de crosta continental extremamente afinada, a qual foi interpretada como crosta proto-oceânica. Estes novos dados demonstram que esta área apresenta fortes similaridades com margens rifteadas não vulcânicas ou pobres em magma.
Several studies have tried to address the evolution of the Atlantic conjugate margins, including Northeast Brazil and West Africa. However, past research advances has been hindered by a lack of data for the marginal region in the eastern portion of northeastern Brazil, extending from the Pernambuco Shear Zone to the Touros High. This situation has imposed serious limitations on the development of a regional view of the geotectonic and paleogeographic evolution of this area and on correlations with regional counterparts in Africa. Here, we present an investigation using regional gravimetric, magnetic and seismic data. The results show that this region represents a basement high with regional orientation of tectonic structures (ENE-WSW) orthogonal at structures developed during the open processes of the Paraíba and Natal Platform Basins (NNE-SSW and NNW-SSE). The continental basement forming a narrow platform with a thin sedimentary cover (0.8-2.5 km) and an abrupt shelf break, which created a large bypass zone towards the slope. The analysis of a deep seismic section revealed that thinned continental crust (transitional crust) occupies a narrow zone and that the continental-oceanic boundary (COB) is located approximately 100 km to the east of the present coastline, at Paraíba Basin, and 70 km, at Natal Platform Basin. Geophysical modeling integrated with interpretation of the seismic data suggests that this region is characterized by an abrupt thinning of continental crust, with an accompanying sudden rise of the Moho. There are also indications for the existence of a zone of extremely thinned continental crust, which was interpreted as protooceanic crust. Our findings suggest that the study area shows strong similarities to nonvolcanic or magma-poor rifted margins.
Brionne, Charles. « Signatures morphosédimentaires de la dynamique juxta-glaciaire à la transition de fronts glaciaires marins à terrestres : le cas de la Côte-Nord du Québec (estuaire et golfe du St Laurent) ». Electronic Thesis or Diss., Strasbourg, 2024. http://www.theses.fr/2024STRAH005.
Texte intégralThis thesis combines a dual geomorphological and sedimentological approach with the use of LiDAR data, bathymetry, drone photogrammetry and radiocarbon dating. It has enabled us to reconstruct the glacial paleodynamics in a deglaciation context for the Laurentide ice sheet since the last glacial maximum, around 20,000 years ago, and more specifically during the transition from an ice margin anchored at sea to a continental ice margin: (1) mapping, synthesising and proposing a model for the megagrooves of the North Shore of the St Lawrence, a first study for these morphologies, and (2) reconstructing the geomorphological and morphosedimentary record of the Pentecôte sedimentary complex, which precisely represents this transition. Overall, this thesis demonstrates the importance of the structural heritage and physiography of the floor at the glacial margin in the reconstruction of the glacial retreat dynamics of the eastern LIS margin
Hamai, Lamine. « Étude thermomécanique de la zone de transition mer-continent de la marge algérienne : implication géodynamique ». Thesis, Nice, 2016. http://www.theses.fr/2016NICE4021/document.
Texte intégralUnderstanding how subduction initiates at a passive margin is a major geodynamic question, which remains debatted because of the forces necessary to overcome bending and frictional resistance of the lithosphere and initiate this subduction. Along the southern shore of the Western Mediterranean Sea, the Algerian margin undergoes ~NS compression due to the African-Eurasian convergence at a rate of less than ~ 1 cm / year. This setting causes tectonic inversion of this North African passive margin and possibly incipient subduction. Indeed, recent geophysical marine data acquired in the Algerian Basin (MARADJA, 2003, 2005MARge Active d’el Djazaïr) and SPIRAL 2009 (Deep Seismic and Regional Investigations in Algeria campaigns) showed evidence of recent compressive deformation. We used SPIRAL wide-angle seismic profiles to determine the state of isostatic equilibrium at the vicinity of the continent-ocean boundary. This allowed us to image a too deep Moho in the oceanic part, and a too shallow one in the continental domain, with a boundary between both domains located at the margin toe. These results indicate that the Algerian margin display the same isostatic anomalies as an active margin. This isostatic disiquilibrium may be simulated by the flexural bending of two lithospheric plates that can be modelled by a finite element procedure. This modeling shows larger vertical deflection in the central part of the study area (6-7 km) compared to the earsternmost and westernmost profiles (3 km)
Walsh, John Patrick. « Continental-margin sedimentation : a wet-tropical perspective from New Guinea / ». Thesis, Connect to this title online ; UW restricted, 2001. http://hdl.handle.net/1773/11017.
Texte intégralPrescott, Clifford Neill. « Marine geophysical investigation of the Hatton Bank volcanic passive continental margin ». Thesis, Durham University, 1988. http://etheses.dur.ac.uk/6660/.
Texte intégralHemer, Mark A. « The oceanographic influence of sedimentation on the continental shelf : a numerical comparison between tropical and Antarctic environments / ». Connect to this title online, 2003. http://adt.lib.utas.edu.au/public/adt-TU20051223.102442.
Texte intégralClose, David Ian. « A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica ». Thesis, University of Oxford, 2005. http://ora.ox.ac.uk/objects/uuid:bfc7eee9-de28-4934-8f79-82b300a5f706.
Texte intégralLivres sur le sujet "Marine to continental transition"
Valentine, Page C. The shelf-slope transition--canyon and upper slope sedimentary processes on the southern margin of Georges Bank : An examination of sedimentary environments in water depths of 150-600 meters and of how they are determined by the interaction of available sediment, bottom currents, and sea-floor morphology. Washington, D.C : U.S. G.P.O., 1987.
Trouver le texte intégralValentine, Page C. The shelf-slope transition--canyon and upper slope sedimentary processes on the southern margin of Georges Bank : An examination of sedimentary environments in water depths of 150-600 meters and of how they are determined by the interaction of available sediment, bottom currents, and sea-floor morphology. Washington, DC : U.S. Geological Survey, 1987.
Trouver le texte intégralUnited States. Minerals Management Service, dir. Outer Continental Shelf : Marine minerals. [Washington, D.C.?] : U.S. Dept. of the Interior, Minerals Management Service, 1992.
Trouver le texte intégralTomoya, Akimichi, dir. Coastal foragers in transition. Osaka : National Museum of Ethnology, 1996.
Trouver le texte intégralWalker, Pam. The continental shelf. New York : Facts on file, 2005.
Trouver le texte intégralWalsh, John Joseph. On the nature of continental shelves. San Diego : Academic Press, 1988.
Trouver le texte intégralPhilippe, Béarez, et Ibarra Santacruz Ángel, dir. Peces marinos del Ecuador continental. Quito : SIMBIOE, 2004.
Trouver le texte intégralSaldanha, Luiz. Fauna submarina Atlântica : Portugal continental, Açores, Madeira. 3e éd. Mem Martins [Portugal] : Publiçacões Europa-América, 1995.
Trouver le texte intégralR, Prothero Donald, Ivany Linda C et Nesbitt Elizabeth R, dir. From greenhouse to icehouse : The marine Eocene-Oligocene transition. New York : Columbia University Press, 2003.
Trouver le texte intégralname, No. From greenhouse to icehouse : The marine Eocene-Oligocene transition. New York : Columbia University Press, 2003.
Trouver le texte intégralChapitres de livres sur le sujet "Marine to continental transition"
Mather, Anne E., et Martin Stokes. « Marine to Continental Transition ». Dans A Field Guide to the Neogene Sedimentary Basins of the Almería Province, SE Spain, 186–224. Oxford, UK : Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444300604.ch5.
Texte intégralMay, Vincent. « Softer Solutions to Coastal Erosion : Making the Transition from Resistance to Resilience ». Dans Coastal Systems and Continental Margins, 1–16. Dordrecht : Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0135-9_1.
Texte intégralGomes, Paulo Otávio, Benedito S. Gomes, Jorge J. C. Palma, Koji Jinno et Jairo M. de Souza. « Ocean-continent transition and tectonic framework of the oceanic crust at the continental margin off NE Brazil : Results of LEPLAC project ». Dans Atlantic Rifts and Continental Margins, 261–91. Washington, D. C. : American Geophysical Union, 2000. http://dx.doi.org/10.1029/gm115p0261.
Texte intégralChakraborty, Nivedita, Subir Sarkar et R. Nagendra. « Continental-to-Marine Transition in an Ongoing Rift Setting : Barremian-Turonian Sediments of Cauvery Basin, India ». Dans Mesozoic Stratigraphy of India, 587–622. Cham : Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71370-6_20.
Texte intégralHay, William W. « Continental Rise ». Dans Encyclopedia of Marine Geosciences, 1–4. Dordrecht : Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6644-0_155-3.
Texte intégralHay, William W. « Continental Slope ». Dans Encyclopedia of Marine Geosciences, 1–5. Dordrecht : Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6644-0_156-3.
Texte intégralHay, William W. « Continental Rise ». Dans Encyclopedia of Marine Geosciences, 122–24. Dordrecht : Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_155.
Texte intégralHay, William W. « Continental Slope ». Dans Encyclopedia of Marine Geosciences, 124–27. Dordrecht : Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_156.
Texte intégralLallemand, Serge. « Active Continental Margin ». Dans Encyclopedia of Marine Geosciences, 1–6. Dordrecht : Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6644-0_102-2.
Texte intégralFujiwara, Yoshihiro, et Koetsu Kon. « Marine Ecology : Continental Shelf to Deep Sea ». Dans Japanese Marine Life, 255–62. Singapore : Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-1326-8_21.
Texte intégralActes de conférences sur le sujet "Marine to continental transition"
Apotrosoaei, V. A., M. Munteanu et D. R. Roban. « Marine to Continental Sedimentary Environment Transition at the Paleogene-Miocene Boundary, South Carpathians Foreland ». Dans 75th EAGE Conference and Exhibition incorporating SPE EUROPEC 2013. Netherlands : EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20131079.
Texte intégralStarratt, Scott W., Jason Addison, Summer Praetorius, David Bukry et Bruce P. Finney. « GULF OF ALASKA CONTINENTAL SHELF – A COMPLICATED GLACIAL TO MARINE TRANSITION IN THE LATE QUATERNARY ». Dans GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383317.
Texte intégralWestgate, Z. J., R. D. Beemer et D. J. DeGroot. « Implications of Glauconite Sands on US Offshore Wind Development ». Dans Innovative Geotechnologies for Energy Transition. Society for Underwater Technology, 2023. http://dx.doi.org/10.3723/unfk6402.
Texte intégralAndeskie, Anna Sofia, et Kathleen C. Benison. « THE PERMIAN HUTCHINSON SALT MEMBER OF KANSAS : MARINE, CONTINENTAL, OR TRANSITIONAL ? » Dans GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322518.
Texte intégralXu, Lifu. « Characteristics and effectiveness evaluation method of marine continental transitional shale reservoir ». Dans Goldschmidt2021. France : European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6961.
Texte intégralWang, Zhuangsen. « Sedimentary control and reservoir response of marine continental transitional shale : Taking the eastern margin of Ordos Basin as an example in China ». Dans Goldschmidt2021. France : European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.4978.
Texte intégralMaurya, V., S. Fontes et E. La Terra. « An Enhanced and Effective Technique for Demarcation of Continental – Oceanic Transition - Application for South Atlantic Conjugate Margins ». Dans 79th EAGE Conference and Exhibition 2017. Netherlands : EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701310.
Texte intégralChu, Daoliang, Jinnan Tong, Michael J. Benton et Haijun Song. « THE CORRELATION OF THE PERMIAN–TRIASSIC TRANSITIONAL BEDS AND MASS EXTINCTION IN CONTINENTAL-MARINE SILICICLASTIC SETTINGS OF WESTERN GUIZHOU AND EASTERN YUNNAN, SOUTHWESTERN CHINA ». Dans GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318745.
Texte intégralHu, Xiao, Yiqun Zhang, Xiaoya Wu, Haizhu Wang et Xu Cui. « A Study on the CO2 Jet Erosion Natural Gas Hydrate with the Influence of Temperature and Confining Pressure ». Dans 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0463.
Texte intégralHan*, Wei-Chung, Char-Shine Liu, Wu-Cheng Chi et Yunshuen Wang. « Structural Inversion and Channel Evolution in a Transition Zone Across the Boundary Between Passive and Active Continental Margins : An Example From Offshore Southwestern Taiwan ». Dans International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2203120.
Texte intégralRapports d'organisations sur le sujet "Marine to continental transition"
Lucking, S. K. The Enduring Mission of the Marine Corps Military Transition. Fort Belvoir, VA : Defense Technical Information Center, février 2009. http://dx.doi.org/10.21236/ada508043.
Texte intégralForkin, Keith A. Proactive Marine Corps Transition Assistance In The Twenty-First Century. Fort Belvoir, VA : Defense Technical Information Center, février 2015. http://dx.doi.org/10.21236/ada620284.
Texte intégralAllen, John S., et Leonard J. Walstad. Assimilation Modeling of Coastal Transition Zone Data and Continental Slope Flow Fields. Fort Belvoir, VA : Defense Technical Information Center, janvier 1991. http://dx.doi.org/10.21236/ada248692.
Texte intégralShapiro, L., B. F. Sherr et E. B. Sherr. Controls on marine carbon fluxes via phytoplankton-mesoplankton interactions in continental shelf waters. Office of Scientific and Technical Information (OSTI), janvier 1992. http://dx.doi.org/10.2172/6430486.
Texte intégralKeen, C. E., et W. Kay. Deep marine multichannel seismic data from the Northeast Newfoundland Continental Margin - Lithoprobe East. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130061.
Texte intégralShapiro, L., B. F. Sherr et E. B. Sherr. Controls on marine carbon fluxes via phytoplankton-mesoplankton interactions in continental shelf waters. Office of Scientific and Technical Information (OSTI), janvier 1992. http://dx.doi.org/10.2172/6525151.
Texte intégralParadis, S., G. J. Simandl, N. Drage, R J D'Souza, D. J. Kontak et Z. Waller. Carbonate-hosted deposits (Mississippi Valley-type, magnesite, and REE-F-Ba) of the southeastern Canadian Cordillera : a review and isotopic data comparison. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/327995.
Texte intégralBennett, Richard H., William B. Sawyer, Donald J. Walter et Eric N. Litman. Pressure Attenuation and Geotechnical Properties in Surficial Marine Sediments : Gulf of Mexico Continental Shelf. Fort Belvoir, VA : Defense Technical Information Center, juin 1992. http://dx.doi.org/10.21236/ada254834.
Texte intégralKay, W. A., et C. E. Keen. Deep marine multichannel seismic reflection data from the Grand Banks, eastern Canadian Continental Margin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130422.
Texte intégralLucatelli, D., J. M. R. Camargo, C. J. Brown, J. F. Souza-Filho, E. Guedes-Silva et T. C. M. Araújo. Marine geodiversity of northeastern Brazil : a step towards benthic habitat mapping in Pernambuco Continental Shelf. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/305889.
Texte intégral