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Artigos de revistas sobre o assunto "Sedimentary bassin"
Robin, Cecile, Francois Guillocheau, Pascal Allemand, Sylvie Bourquin, Gilles Dromart, Jean-Michel Gaulier e Christophe Prijac. "Echelles de temps et d'espace du controle tectonique d'un bassin flexural intracratonique; le bassin de Paris". Bulletin de la Société Géologique de France 171, n.º 2 (1 de março de 2000): 181–96. http://dx.doi.org/10.2113/171.2.181.
Texto completo da fonteYelles-Chaouche, A. K., R. Ait Ouali, R. Bracene, M. E. M. Derder e H. Djellit. "Chronologie de l'ouverture du bassin des Ksour (Atlas Saharien, Algerie) au debut du Mesozoique". Bulletin de la Société Géologique de France 172, n.º 3 (1 de maio de 2001): 285–93. http://dx.doi.org/10.2113/172.3.285.
Texto completo da fonteCyrille, Yao Kouadio, Kouassi Kouamé Alfred, Boga Atabli Hervé, Monde Sylvain, Digbehi Zéli Bruno e N’da Loukou Victor. "Contribution A La Caracterisation Diagraphique Des Depots Carbonates Du Cretace Du Bassin Sedimentaire De Cote D’ivoire". European Scientific Journal, ESJ 12, n.º 33 (30 de novembro de 2016): 391. http://dx.doi.org/10.19044/esj.2016.v12n33p391.
Texto completo da fonteHughes, K. Stephen, James P. Hibbard, Jeffrey C. Pollock, David J. Lewis e Brent V. Miller. "Detrital Zircon Geochronology Across the Chopawamsic Fault, Western Piedmont of North-Central Virginia: Implications for the Main Iapetan Suture in the Southern Appalachian Orogen". Geoscience Canada 41, n.º 4 (3 de dezembro de 2014): 503. http://dx.doi.org/10.12789/geocanj.2014.41.052.
Texto completo da fonteDurlet, Christophe, e Jacques Thierry. "Modalites sequentielles de la transgression aaleno-bajocienne sur le sud-est du Bassin parisien". Bulletin de la Société Géologique de France 171, n.º 3 (1 de maio de 2000): 327–39. http://dx.doi.org/10.2113/171.3.327.
Texto completo da fonteSurmely, Frédéric. "Characterization of Tertiary Flints by geochemistry; application to the French territory". Lietuvos archeologija Lietuvos archeologija T. 46 (18 de dezembro de 2020): 191–206. http://dx.doi.org/10.33918/25386514-046007.
Texto completo da fonteFarki, Khadija, Ghalem Zahour, Youssef Zerhouni e Hamid Wafa. "Contribution to the Understanding of the Sedimentary and Tectono-Volcanic Evolution of Triassic and Liassic Series of Oued N’Fifikh (Coast Meseta, Morocco)". Annales de la Société Géologique du Nord, n.º 19 (1 de dezembro de 2012): 145–56. http://dx.doi.org/10.54563/asgn.1479.
Texto completo da fonteCousineau, Pierre A., e Pierre St-Julien. "Stratigraphie et paléogéographie d'un bassin d'avant-arc ordovicien, Estrie-Beauce, Appalaches du Québec". Canadian Journal of Earth Sciences 31, n.º 2 (1 de fevereiro de 1994): 435–46. http://dx.doi.org/10.1139/e94-040.
Texto completo da fonteN’zi, Jean Claude, Mamadou Toure, N’goran Jean-Paul Yao, Rachelle Affouet Kouassi, Zeli Bruno Digbehi e Kouamé Aka. "Caracterisation Sedimentologique Et Mineralogique Des Formations Tertiares Du Bassin Onshore De La Region D’abidjan, Cote d’Ivoire". European Scientific Journal, ESJ 14, n.º 18 (30 de junho de 2018): 218. http://dx.doi.org/10.19044/esj.2018.v14n18p218.
Texto completo da fonteNZALI, Timothée, Jean-Clair DUCHESNE, Christiane JACQUEMIN e Jacqueline VANDER AUWERA. "Pyrométamorphisme induit par la gazéification souterraine de niveaux charbonneux du Westphalien dans le bassin de Mons (Belgique) [Pyrometamorphism induced by underground coal gasification of Westphalian beds in the Mons basin (Belgium)]". Geologica Belgica 2, n.º 3-4 (1 de junho de 2000): 221–34. http://dx.doi.org/10.20341/gb.2014.020.
Texto completo da fonteTeses / dissertações sobre o assunto "Sedimentary bassin"
Paquet, Fabien. "Evolution morphostructurale des bassins de marge active en subduction : l'exemple du bassin avant arc de Hawke Bay en Nouvelle-Zélande = Morphostructural evolution of active subduction margin basins : the example of the Hawke Bay forearc basin, New Zealand /". Rennes : CNRS, Université de Rennes, 2008. http://library.canterbury.ac.nz/etd/adt-NZCU20080225.224857.
Texto completo da fonte"Thése de Doctorat de l'Université de Rennes 1 réalisée en co-tutelle avec l'Université de Canterbury (Christchurch, Nouvelle-Zélande)." "Soutenue le 9 novembre 2007." Includes bibliographical references. Also available via WWW.
Razafimbelo, Eugène. "Le bassin de morondava (madagascar) : synthese geologique et structurale". Université Louis Pasteur (Strasbourg) (1971-2008), 1987. http://www.theses.fr/1987STR13184.
Texto completo da fonteHeilbronn, Gloria. "Évolution paléogéographique et paléotopographique du Tian Shan Chinois au Mésozoïque". Thesis, Rennes 1, 2014. http://www.theses.fr/2014REN1S112/document.
Texto completo da fonteThe Tian Shan is an intracontinental range located in Central Asia. The structure of the range formed during the Paleozoic through the accretion of several blocks. Recently the range has been reactivated due to far-field effects of the collision between India and Asia. The topographic and tectonic evolution of the range in-between these two major relief-building phases (Late Paleozoic and Cenozoic) is still poorly understood. Two different approaches are combined in this work, in order to determine the Mesozoic topographic evolution of the area, in a qualitative way.The Late-Paleozoic range has been progressively eroded until the Upper Triassic/Lower Jurassic. Tectonic activity was relatively quiet during the Jurassic characterised by low exhumation rates. We suggest that the tectonic regime was dominated by transtension in the Tian Shan area. This period is linked to a regional peneplanation in Central Asia. At the Jurassic-Cretaceous boundary, the occurrence of alluvial fan deposits shows a reactivation of the range, though not strong enough to be recorded by low-temperature thermochronology. This period is characterised by an overall extensional tectonic regime all over Central Asia, with the opening of the Caspian Basin further west. It precedes the phase of very slow exhumation that occurs during the Lower Cretaceous. From 100 Ma and during the Upper Cretaceous, the range is progressively reactivated. We suggest that this correspond to a delayed answer of the Lhassa bloc collision (140 - 120 Ma). Around 65 - 60 Ma, a new phase of rapid exhumation attests of a stronger reactivation, localised along the major faults. This is contemporary of bloc collisions along the south-west margin of Asia, such as the Kohistan Block, the Dras arc or the Afghan Block. In the Tian Shan area, the development of calcrete features in the Paleocene suggests the end of tectonic activity, before the new reactivation in the Neogene.The combination of low temperature thermochronology on the basement rocks and facies sedimentology in the various basins indicate that while during the Mesozoic, the Palaeo-Tian Shan topography generally flattens, some small-scale tectonic events driven by far-field effects of major geodynamic processes around the edges of Asia did occur. However, those tectonic movements did not induce enough exhumation to be recorded by low temperature thermochronometers. Only the sediment record allows their detection and detailed description
Xia, Wenjing. "Sedimentary and structural characteristics of the Triassic Nanpanjiang Basin (Southwest China). New insights on the regional tectonic evolution". Thesis, Orléans, 2018. http://www.theses.fr/2018ORLE2040/document.
Texto completo da fonteRanks as the largest sedimentary basin in the South China during the Triassic, The Nanpanjiang basin attracts a large attention of the geology community for a long time. After many years study, there still exist several debates on i) the provenance of the sedimentary detritus, ii) the time of the change of the tectonic regime from extension to compression, iii) the type of the basin and its geodynamic background. In this thesis, a multidisciplinary study including analysis of sedimentary facies, paleo-current, frame work detritus mode, heavy mineral combinations and their geochemistry feature, rock magnetism and Zircon-baddeleyite isotopic dating on diabase was conducted to rebuild the evolution of the basin.The results show a three-stage evolution, i) during the Late Permian to the Early Triassic, the 269Ma diabase intruding into the basin announces the opening of the basin, the sedimentary environment became deeper. ii) During the late stage of the Early Triassic (~245 Ma) to the Middle Triassic, owing to the influences of the Xuefengshan orogen and the Indochina orogen which are located to the east and south of the basin, the basin evolved into a foreland basin. The diabase ceased emplacement in this period. The detritus and paleo-current analysis indicate that during this stage, the provenances of the East part and the South part of the basin were Xuefengshan Orogen and Indochina Orogen respectively. iii) During the Late Tirassic, the depth of the sedimentary environment decrease drasticly, indicating that the basin began to shrink owing to the compression of the Xuefengshan Orogen and the Indochina Orogen
Haile-Meskale, Mezmure. "Une étude intégrée de la quantité et de la qualité de l'eau souterraine dans la partie basse du bassin de la Santa Lucia, Uruguay /". Thèse, Montréal : Université du Québec à Montréal, 1990. http://theses.uqac.ca.
Texto completo da fonteCette thèse à été réalisée à l'Université du Québec à Montréal dans le cadre du programme de doctorat en ressources minérales extensionné de l'Université du Quebec à Chicoutimi. CaQCU Document électronique également accessible en format PDF. CaQCU
Monnier, Damien. "Dynamique de mise en place des réseaux d'intrusions sableuses dans les bassins sédimentaires : impact sur l'évolution post-dépôt des réservoirs et le réseau de migration associé". Thesis, Montpellier 2, 2013. http://www.theses.fr/2013MON20006.
Texto completo da fonteSand intrusions (or injectites) are most often the product of post-depositional remobilization of sand leading to its injection into the surrounding rocks. While injectites were recognized for the first time nearly 200 years ago, their emplacement process has been studied for a couple of decades only, since the concepts of deep sea depositional environments have allowed us to better understand their emplacement processes. However, these processes are still relatively poorly understood. Our approach is based on the study of injectites in the Lower Congo Basin from seismic and well data, which we compare to a fossil system in the SE France basin. We have shown that:(1) In buried turbidite channel systems draping deposits on the channel flanks and terraces of channels have the same geophysical signature as ‘wing-like' injectites. Finally, the only criterion for identifying seismic injectites is the presence of bedding-discordant seismic reflections, and in the best case the associated uplift of the overlying seismic reflectors.(2) Seismic-scale conical and saucer-shaped sand injectites have been identified in the Lower Congo Basin. The remobilization is likely due to overpressuring induced by the buoyancy effect of hydrocarbons trapped in the margins of a lobe buried underneath 160 m of sediment, followed by the sudden injection of fluidized sand associated with fault reactivation of faults (with a possible role of nearby salt diapirs).(3) A network of injectites (dykes, sills/wings and laccoliths) was formed in the Vocontian basin during the late Albian and/or early Cenomanian, from a lower-middle Albian turbidite channel. The emplacement is probably due to the early compartmentalization of the channel during its burial and the increase of the sedimentation rate generating overpressure; and the subsequent large influx of deep fluids triggering injection. The injection of sand was polyphased: a first episode formed the sills and another emplaced the dykes. Sills/wings and dykes propagated about 2 km laterally away from the parent sand body and about 200 m up to the surface, revealing a much more extended lateral than vertical reach, contrary to the classically accepted idea from the interpretation of seismic data.(4) The emplacement of this large network of injectites was governed by hydrofracturing. Therefore, its morphology is dependent on the host rock heterogeneity (isotropy, fractures), the paleo-stress orientation (σ3 = NW-SE) and the burial depth of the source (300-600 m) at the time of injection. The study of this fossil network allows us to define the relationship between morphology of the injected network and stress state at the time of injection. This relationship can be extrapolated to constrain the morphology of subsurface networks beyond seismic visibility.(5) Sands injected into low permeability lithologies bear evidence to a major event of fluid escape in the studied basin, but also channeled fluids long after their formation. In this way, injectites both attest to specific episodes of fluid migration in sedimentary basins and contribute to long-lived re-routing of migrating fluids once emplaced.The injection of sand is associated with the sudden escape of fluids, probably resulting from a significant tectonic and/or sedimentary event; in addition, the architecture of injectite networks is governed by the local paleo-stress and heterogeneity in the host rock. Consequently, characterizing injectite networks is an important step in understanding the plumbing systems of continental margins, i.e. the post-depositional evolution of sedimentary basins
Pegaz-fiornet, Sylvie. "Etude de modèles pour la migration des hydrocarbures dans les simulateurs de bassin". Thesis, Aix-Marseille 1, 2011. http://www.theses.fr/2011AIX10049.
Texto completo da fonteHydrocarbon migration modeling in sedimentary basins aims to localize and to quantify hydrocarbon accumulations in geological formations in order to estimate their petroleum potential. In this thesis, we study “Darcy” migration models and also simplified migration models such as “ray-tracing” and “invasion percolation”; the purpose is to conduct a critical analysis and to offer improvements while providing a guide for a relevant use on case studies.We start by a review of migration mechanisms from the pore scale to the basin scale, then we present each model.In a following part, we propose two invasion percolation algorithms: the first one is suited to structured grids, the second one allows to take better account of unstructured grids.In a third part, we take an interest in the comparison between the different models and particularly between “Darcy” and “invasion percolation” approaches. First we devote our attention to numerical aspects supported by several use cases; then we realize a formal comparison by studying the asymptotic limit of the “Darcy” model large time solution. Afterwards, we present several applications including the study of a 3D real case in complex geometry.Finally, we conclude this work with two articles. The first one shows an evolution of “Darcy” models by using the method of local grid refinement with an illustration on a case study from northern Kuwait. The second one synthesizes the main results on “Darcy” and “invasion percolation” methods
Oh, Chun Hyuck. "Géochimie minérale et organique et métallogénie du gisement uranifère de Goesan, bassin d'Ogcheon (Corée)". Orléans, 1986. http://www.theses.fr/1986ORLE3030.
Texto completo da fonteDentzer, Jacques. "Forçages environnementaux et contrôles structuraux sur le régime thermique actuel du bassin de Paris : enjeux pour la compréhension du potentiel géothermique en Ile-de-France". Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066187/document.
Texto completo da fonteThe acquisition of measurements of temperature and of thermal conductivity has enriched the understanding of the thermal regime of the Paris sedimentary basin and brought to light spatial and temporal thermal heterogeneities. In order to understand them better, these variations need to be integrated into a multidisciplinary vision of the basin by comparing data against models. The bibliographic review made it possible to integrate data of diverse sorts, to compare them using GIS and to investigate the knowledge base. This study has highlighted and reinterpreted the vertical variations of geothermal flux. Simulations carried out based on diffusive palaeoclimatic scenarios show that the system has retained a memory of the effects of palaeoclimates. Furthermore, for the first time, a systematic decline of the geothermal flux has been identified at the level of the main aquifer formations. Transitory thermo-hydraulic simulations of palaeoclimatic phenomena show the development in the sedimentary basin of cold and hot zones according to the areas of flow. An explanation of the temperature anomaly of over 20°C between the geothermal installations located to the north and south of Paris in the Bathonian is put forward. The models produced clearly show the potential contribution of fractured zones, as well as that of the faults, to the heterogeneity observed in the temperature field of the basin by allowing flow constrained by the regional charge gradient and unstable densities. This work has shown the link between the formations in the basin which are exploited for their resources or used as a storage medium
Laurent, Dimitri. "Marqueurs de la dynamique des fluides associée à l'enfouissement des bassins sédimentaires : Exemples du Bassin Permien de Lodève (France) et du North Viking Graben (Mer du Nord)". Thesis, Montpellier, 2015. http://www.theses.fr/2015MONTS170/document.
Texto completo da fonteThis work focus on the characterization of the source and dynamic of compactional fluids during sedimentary burial, through two complementary examples of late orogenic oil-field half-grabens: The exhumed Lodève Permian Basin and a deep buried Jurassic basin in the North Viking Graben (North Sea).Constituting the main part of the thesis, a multi-disciplinary approach was conducted in the Lodève Basin where Ba-F-Cu-Pb polymetalic mineralized systems are trapped into synrift faults and paleokarsts in the carbonate basement at the hinge point of the roll-over. The source, timing and P/T conditions of fluid migration were deduced from the analysis of the microfabric, the fluid inclusions microthermometry, and the isotopic (Sr, S, O, H) and Rare Earth Element (REE) signature. Results are then crossed with a structural and thermal modeling that consolidates the sequence and dynamics of fluid during burial.A similar approach was conducted in the North Viking Graben where fluid markers are restricted to 3D seismic and well core data. Comparable Ba-Pb-Zn veins are reported in basin margin, plugging one of the most important siliciclastic hydrocarbon reservoir in the substratum. This analysis provides additional constraints on basinal fluid behavior and allows us to propose a global dynamic model for various compositions of fluids and reservoirs.We conclude to a polyphase fluid sequence history including:(a) In the carbonate basement of the Lodève Basin, karstic paleocanyon incisions and associated cavities coupled to synrift fault, act as major drain for fluids. These structures are early affected by hypogen-sulfuric karstification in response to the interaction between bacterial oxidation of sulfides entrapped within Lower Permian blackshales and the basement oxidizing aquifer.(b) Disequilibrium compaction initiates overpressure-driven basinal fluid migration towards basin margins, characterized by temperatures around 150-180°C and salinities between 9 et 18wt%eq.NaCl. Isotopic (Sr, S, O) and REE analyses reveal that Ba-M+-rich mineralizing fluids derived mainly from buried blackshales diagenesis. External Fluids coming from the lower crust are also identified that play a key role in fluorite precipitation by the leaching of late hercynian granites (mean temperature of 250°C and salinity > 20wt%eq.NaCl).(c) During the synrift period, fluid overpressure is responsible for the periodic reactivation of fault plane according to seismic-valve process, bedded-control shearing and hydraulic brecciation at the basement-seal interface. These mechanisms induce cyclic polymetallic mineralization by the mixing between in situ formation water and deep ascending basinal fluids.(d) Thermogenic fluids expulsion starts with last basinal fluids during late burial stage. Hydrocarbons thus migrate along the same regional pathways up to the rollover crest, where they are partly rerouted by the previous mineralized baffle.(e) In the Lodève basin, post-rift exhumation of the margins led to the remobilization of synrift deposits by subaerial biochemical processes at the sulfate-methane transition. The latter results from the interaction between the still active hydrocarbon dysmigration with a playa lake sulfate-rich aquifer. Secondary low-temperature barite fronts precipitate then within basement meteoric karsts.In addition to the « source to sink » model of basinal fluids, this work provides new insights on the early plugging of hydrocarbon reservoirs and for the metallogenesis of Mississippi Valley-Type deposits
Livros sobre o assunto "Sedimentary bassin"
Fries, Gérard. Dynamique du bassin subalpin méridional de l'Aptien au Cénomanien. Paris: Ecole des mines de Paris, Centre de géologie générale et minière, 1987.
Encontre o texto completo da fonteDeurbergue, Arnaud. Transformations post-sédimentaires sur la bordure nord du Massif Central: Les formations ferrugineuses du bassin de Chaillac, le quartz carrié des environs de La Châtre, les altérites siliceuses du bassin de Cosne d'Allier. Orléans: Editions du Bureau de recherches géologiques et minières, Service géologique national, 1985.
Encontre o texto completo da fonteStratigraphie séquentielle du Crétacé supérieur du bassin vocontien occidental (sud-est France): Comparaison avec d'autres bassins. Villeurbanne, France: Centre des sciences de la terre, Université Claude-Bernard-Lyon I, 1994.
Encontre o texto completo da fonteI, Galushkin Yu, ed. Basin analysis and modeling of the burial, thermal and maturation histories in sedimentary basins. Paris, France: Editions Technip, 2005.
Encontre o texto completo da fonteVidal, Olivier. Contribution géophysique à la reconnaissance structurale d'un bassin sédimentaire par la magnétotellurique, d'un segment de la chaîne hercynienne (Cézallier, Massif Central français) par la gravimétrie. Montpellier, France: Centre géologique et géophysique, Université des sciences et techniques du Languedoc, 1986.
Encontre o texto completo da fonteQuantitative sedimentary basin modeling. Tulsa, Okla: American Association of Petroleum Geologists, 1990.
Encontre o texto completo da fonteMiall, Andrew D. Principles of Sedimentary Basin Analysis. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4757-4235-0.
Texto completo da fonteMiall, Andrew D. Principles of Sedimentary Basin Analysis. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-03999-1.
Texto completo da fontePrinciples of sedimentary basin analysis. 3a ed. Berlin: Springer, 2000.
Encontre o texto completo da fontePrinciples of sedimentary basin analysis. 2a ed. New York: Springer-Verlag, 1990.
Encontre o texto completo da fonteCapítulos de livros sobre o assunto "Sedimentary bassin"
Scheck-Wenderoth, Magdalena. "Sedimentary Basins". In Encyclopedia of Solid Earth Geophysics, 1–13. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10475-7_216-1.
Texto completo da fonteJelgersma, Saskia. "Sedimentary Basins". In Encyclopedia of Earth Sciences Series, 1517–23. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_280.
Texto completo da fonteJelgersma, Saskia. "Sedimentary Basins". In Encyclopedia of Earth Sciences Series, 1–7. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_280-2.
Texto completo da fonteScheck-Wenderoth, Magdalena. "Sedimentary Basins". In Encyclopedia of Solid Earth Geophysics, 1059–70. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_216.
Texto completo da fonteHealy, Terry R., Katherine Stone, Orville Magoon, Billy Edge, Lesley Ewing, Andrew D. Short, Dougals L. Inman et al. "Sedimentary Basins". In Encyclopedia of Coastal Science, 853–59. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_280.
Texto completo da fonteScheck-Wenderoth, Magdalena. "Sedimentary Basins". In Encyclopedia of Solid Earth Geophysics, 1353–65. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_216.
Texto completo da fonteKundu, Sandeep Narayan. "Sedimentary Basins". In Geoscience for Petroleum Engineers, 33–42. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-7640-7_3.
Texto completo da fonteEinsele, Gerhard. "Basin Evolution and Sediments". In Sedimentary Basins, 543–643. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04029-4_12.
Texto completo da fonteEinsele, Gerhard. "Basin Evolution and Sediments". In Sedimentary Basins, 429–506. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77055-5_12.
Texto completo da fonteJayko, Angela S., e Marcus Bursik. "Active Transtensional Intracontinental Basins: Walker Lane in the Western Great Basin". In Tectonics of Sedimentary Basins, 226–48. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781444347166.ch11.
Texto completo da fonteTrabalhos de conferências sobre o assunto "Sedimentary bassin"
Feng, Zhiqiang, Gao Dengliang, Stephan A. Graham, Wu Gaokui e Duan Taizhong. "Classification of sedimentary basins". In International Meeting for Applied Geoscience & Energy. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2023. http://dx.doi.org/10.1190/image2023-3917017.1.
Texto completo da fonteBasani, R., T. E. Aas, E. W. Hansen e J. Howell. "Numerical Simulations of Sedimentation and Compaction of Turbiditic Sand at Reservoir Scale in the Peïra Cava Sub Basin". In Second Conference on Forward Modelling of Sedimentary Systems. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600376.
Texto completo da fonteNimmagadda, Shastri L., Heinz Dreher, Andi Noventianto, Aswin Mustoffa e Parapaty Halley. "Sedimentary basin - A petroleum digital ecosystem". In 2013 IEEE 11th International Conference on Industrial Informatics (INDIN). IEEE, 2013. http://dx.doi.org/10.1109/indin.2013.6622942.
Texto completo da fonteM. Shannon, P., I. K. Sinclair, B. J. P. Williams, S. D. Harker e J. G. Moore. "Tectonic control and sedimentary basin evolution of three mesozoic basins, N. Atlantic borderlands". In 55th EAEG Meeting. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609.201411805.
Texto completo da fonteRupke, L., D. W. Schmid, S. M. Schmalholz e Y. Y. Podladchikov. "Uplift in Sedimentary Basins Revisited - New Insights from the Voring Basin, Norwegian Sea". In 1st International Petroleum Conference and Exhibition Shiraz 2009. Netherlands: EAGE Publications BV, 2009. http://dx.doi.org/10.3997/2214-4609.20145871.
Texto completo da fonteShyu, Chase J., Eh Tan, Pin-Rong Wu, Kenn-Ming Yang e Andrew T. Lin. "RELATIONSHIP AMONG BASIN EVOLUTION, FAULT ACTIVITY, AND SYN-RIFT SEDIMENTARY STRATA: INSIGHTS FROM THERMO-MECHANICAL MODELING OF RIFTED SEDIMENTARY BASINS". In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-392454.
Texto completo da fonteMboya, V. E. "Sedimentary Basins Prospective for Hydrocarbons". In Third EAGE Eastern Africa Petroleum Geoscience Forum. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201702431.
Texto completo da fonteLawrence, David T., Mark Doyle, Sigmund Snelson e W. T. Horsfield. "Stratigraphic modeling of sedimentary basins". In SEG Technical Program Expanded Abstracts 1987. Society of Exploration Geophysicists, 1987. http://dx.doi.org/10.1190/1.1891985.
Texto completo da fontePakhomova, K. A., e D. K. Drozdov. "PALEOGEOGRAPHY OF THE SUKHANSK SEDIMENTARY BASIN BASED ON PALEOMAGNETIC DATA OF KHATYSPYT FORMATION (VENDIAN OF OLENEK UPLIFT)". In All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Trofimuk Readings - 2021. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1251-2-33-37.
Texto completo da fonteAstakhov, S. M., e A. N. Reznikov. "Geothermal Regimes of the World Sedimentary Basins and Thermal Evolution in Basin Modeling Software". In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142731.
Texto completo da fonteRelatórios de organizações sobre o assunto "Sedimentary bassin"
Dewing, K. E., C. J. Lister, L. E. Kung, E. A. Atkinson, H. M. King, A. M. Kalejaiye e A. Krakowka. Hydrocarbon resource assessment of Hudson Bay, northern Canada. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332028.
Texto completo da fonteYuen, David A. Physical Modelling of Sedimentary Basin. Office of Scientific and Technical Information (OSTI), abril de 2003. http://dx.doi.org/10.2172/899950.
Texto completo da fonteMossop, G. D., K. E. Wallace-Dudley, G. G. Smith e J. C. Harrison. Sedimentary basins of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215559.
Texto completo da fonteBell, J. S. Stress in Sedimentary Basins Seminar. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130791.
Texto completo da fonteSyvitski, J. P. M. Modelling the sedimentary fill of basins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128089.
Texto completo da fonteDiecchio, R. J. Taconian Sedimentary Basins of the Appalachians. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132191.
Texto completo da fontePeter J. Ortoleva. Self-Organized Megastructures in Sedimentary Basins. Office of Scientific and Technical Information (OSTI), junho de 2004. http://dx.doi.org/10.2172/825402.
Texto completo da fonteGrasby, S. E., e J. M. Galloway. Rare-earth elements of Permian through Cretaceous strata of the Sverdrup Basin, Nunavut and Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330202.
Texto completo da fonteThaddeus S. Dyman, Troy Cook, Robert A. Crovelli, Allison A. Henry, Timothy C. Hester, Ronald C. Johnson, Michael D. Lewan et al. NATURAL GAS RESOURCES IN DEEP SEDIMENTARY BASINS. Office of Scientific and Technical Information (OSTI), fevereiro de 2002. http://dx.doi.org/10.2172/833232.
Texto completo da fonteMorrow, D. W. Devonian of the Northern Canadian Mainland Sedimentary Basin (a contribution to the Geological Atlas of the northern Canadian Mainland Sedimentary Basin). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/290970.
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