Thematische Bibliographien / Continental Rift of Southern Brazil

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Auswahl der wissenschaftlichen Literatur zum Thema „Continental Rift of Southern Brazil“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 5. Februar 2022

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Zeitschriftenartikel zum Thema "Continental Rift of Southern Brazil"

Reuber, Kyle, and Paul Mann. "Control of Precambrian-to-Paleozoic orogenic trends on along-strike variations in Early Cretaceous continental rifts of the South Atlantic Ocean." Interpretation 7, no. 4 (2019): SH45—SH69. http://dx.doi.org/10.1190/int-2018-0257.1.

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The Early Cretaceous (135–130 Ma) continental rupture of Western Gondwana to form the South American and African plates closely paralleled the elongate trends of Precambrian and Paleozoic orogenic belts. These orogenic belts were produced as a result of the Neoproterozoic convergent and strike-slip assembly of Gondwana that redeformed during later, Paleozoic orogenic events. Continued continental rifting led to the formation of conjugate, South Atlantic volcanic passive margins whose widths vary from 55 to 180 km. Along-strike variations in crustal stretching, as measured from deep-penetration

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SAALMANN, K., M. V. D. REMUS, and L. A. HARTMANN. "Structural evolution and tectonic setting of the Porongos belt, southern Brazil." Geological Magazine 143, no. 1 (2006): 59–88. http://dx.doi.org/10.1017/s0016756805001433.

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The SW–NE-striking Porongos belt, located between juvenile Neoproterozoic rocks in the west and the Dom Feliciano belt, characterized by intense reworking of older crust, in the east, comprises a greenschist to amphibolite-facies metavolcano-metasedimentary succession (Porongos sequence) of unknown age with some exposures of Palaeoproterozoic gneisses (Encantadas gneisses). High-temperature ductile deformation of the basement gneisses comprises at least two magmatic events followed by three deformational phases including folding and shearing (DT1–DT3) and can be attributed to the Palaeoprotero

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MENEZES, NAÉRCIO A., ALEXANDRE C. RIBEIRO, STANLEY WEITZMAN, and RODRIGO A. TORRES. "Biogeography of Glandulocaudinae (Teleostei: Characiformes: Characidae) revisited: phylogenetic patterns, historical geology and genetic connectivity." Zootaxa 1726, no. 1 (2008): 33. http://dx.doi.org/10.11646/zootaxa.1726.1.3.

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The biogeography of the Glandulocaudinae (former Glandulocaudini) is reviewed. The major pattern of diversification presented by this group of freshwater fishes can be clearly associated to the main aspects of the tectonic evolution of the southern portion of the Cis-Andean South American Platform. The phylogenetic relationships within the group suggest that the clade represented by Lophiobrycon is the sister-group of the more derived clade represented by the genus Glandulocauda and Mimagoniates. Lophiobrycon and Glandulocauda occur in areas of the ancient crystalline shield of southeastern Br

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Green, Paul F., Karna Lidmar-Bergström, Peter Japsen, Johan M. Bonow, and James A. Chalmers. "Stratigraphic landscape analysis, thermochronology and the episodic development of elevated, passive continental margins." Geological Survey of Denmark and Greenland (GEUS) Bulletin 30 (December 30, 2013): 1–150. http://dx.doi.org/10.34194/geusb.v30.4673.

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The continental margin of West Greenland is similar in many respects to other elevated, passive continental margins (EPCMs) around the world. These margins are characterised by extensive regions of low relief at elevations of 1–2 kilometres above sea level sloping gently inland, with a much steeper, oceanward decline, often termed a 'Great Escarpment', terminating at a coastal plain. Recent studies, based on integration of geological, geomorphological and thermochronological evidence, have shown that the high topography of West Greenland was formed by differential uplift and dissection of an O

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Franco-Magalhaes, A. O. B., P. C. Hackspacher, U. A. Glasmacher, and A. R. Saad. "Rift to post-rift evolution of a “passive” continental margin: the Ponta Grossa Arch, SE Brazil." International Journal of Earth Sciences 99, no. 7 (2010): 1599–613. http://dx.doi.org/10.1007/s00531-010-0556-8.

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Peace, Alexander L., and J. Kim Welford. "Conjugate margins — An oversimplification of the complex southern North Atlantic rift and spreading system?" Interpretation 8, no. 2 (2020): SH33—SH49. http://dx.doi.org/10.1190/int-2019-0087.1.

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The prevalence of conjugate margin terminology and studies in the scientific literature is testimony to the contribution that this concept and approach has made to the study of passive margins, and more broadly extensional tectonics. However, when applied to the complex rift, transform, and spreading system of the southern North Atlantic (i.e., the passive margins of Newfoundland, Labrador, Ireland, Iberia, and southern Greenland), it becomes obvious that at these passive continental margin settings, additional geologic phenomena complicate this convenient description. These aspects include (1

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de Castro, D. L., and F. H. R. Bezerra. "Fault evolution in the Potiguar rift termination, Equatorial margin of Brazil." Solid Earth Discussions 6, no. 2 (2014): 2885–913. http://dx.doi.org/10.5194/sed-6-2885-2014.

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Abstract. The transform shearing between South American and African plates in the Cretaceous generated a series of sedimentary basins on both plate margins. In this study, we use gravity, aeromagnetic, and resistivity surveys to identify fault architecture and to analyse the evolution of the eastern Equatorial margin of Brazil. Our study area is the southern onshore termination of the Potiguar rift, which is an aborted NE-trending rift arm developed during the breakup of Pangea. The Potiguar rift is a Neocomian structure located in the intersection of the Equatorial and western South Atlantic

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Rohais, Sébastien, Sébastien Joannin, Jean-Paul Colin, Jean-Pierre Suc, François Guillocheau, and Rémi Eschard. "Age and environmental evolution of the syn-rift fill of the southern coast of the gulf of Corinth (Akrata-Derveni region, Greece)." Bulletin de la Société Géologique de France 178, no. 3 (2007): 231–43. http://dx.doi.org/10.2113/gssgfbull.178.3.231.

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Abstract The southern coast of the gulf of Corinth exhibits syn-rift deposits, giving insights into the first stages of continental extension as well as the geodynamic evolution of the surrounding Aegean region. The stratigraphy (relative position, 3D geometry, dating) of these deposits is still subject to controversies. The syn-rift evolution of the central part of the southern coast of the Corinth rift is revisited, based on new sedimentological and paleontological data. While ostracods analysis provides precise information about the paleoenvironments, recent advances in palynology supply a

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Zavialov, Peter O., Sonia M. F. Gianesella-Galvão, Felipe M. Pimenta, Guilherme P. Castelão, and Sanjar M. Abdoullaev. "Diurnal variability on the continental shelf of Southern Brazil." Continental Shelf Research 20, no. 1 (2000): 15–35. http://dx.doi.org/10.1016/s0278-4343(99)00040-0.

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de Castro, D. L., and F. H. R. Bezerra. "Fault evolution in the Potiguar rift termination, equatorial margin of Brazil." Solid Earth 6, no. 1 (2015): 185–96. http://dx.doi.org/10.5194/se-6-185-2015.

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Abstract. The transform shearing between South American and African plates in the Cretaceous generated a series of sedimentary basins on both plate margins. In this study, we use gravity, aeromagnetic, and resistivity surveys to identify architecture of fault systems and to analyze the evolution of the eastern equatorial margin of Brazil. Our study area is the southern onshore termination of the Potiguar rift, which is an aborted NE-trending rift arm developed during the breakup of Pangea. The basin is located along the NNE margin of South America that faces the main transform zone that separa

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Dissertationen zum Thema "Continental Rift of Southern Brazil"

Muniz, Moises Calazans. "Tectono-stratigraphic evolution of the Barremian-Aptian continental rift carbonates in southern Campos Basin, Brazil." Thesis, Royal Holloway, University of London, 2013. http://repository.royalholloway.ac.uk/items/3f728d6a-29d2-41ab-9a5a-fec206df679b/1/.

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The southern Campos Basin comprises syn- and post-rift strata characterised by thick and extensive units of non-marine limestones. These carbonate platforms are scientifically significant due to their unusual palaeoenvironmental setting, and the complexity of the factors controlling their accumulation. They are of economic importance due to discoveries of giant hydrocarbon accumulations in these non-marine carbonate rocks. 3D seismic interpretations show an oblique extensional rifting system that formed a series of graben, half-graben, accommodation zones and horsts oriented NESW to NNE-SSW. T

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Silva, Rafael Monteiro da. "Modelagem numérica do padrão de esforços na litosfera e implicações na formação do Rifte Continental do Sudeste do Brasil." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/14/14132/tde-25052018-141852/.

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O Rifte Continental do Sudeste do Brasil é uma das feições geotectônicas mais expressivas da margem continental brasileira e sua formação influenciou significativamente o padrão de transporte de sedimentos para as bacias marginais de Santos e Campos. Diferentes modelos foram propostos para a origem deste rifte e envolvem a reativação, como falhas normais, de zonas de cisalhamento Pré-Cambrianas. Não obstante, esses modelos são qualitativos e não existem experimentos numéricos que avaliaram a viabilidade dos mecanismos propostos para a origem do rifte. O presente trabalho teve como objetivo es

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Peate, David William. "Stratigraphy and petrogenesis of the Parana continental flood basalts, southern Brazil." Thesis, Open University, 1989. http://oro.open.ac.uk/57282/.

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The Early Cretaceous (-130 Ma) Parana lavas of South America represent the largest preserved example of a continental flood basalt (CFB) province, with a present area in excess of 1.2 x 106 km2. Magmatism is dominated by tholeiitic basalts (> 90 %), with minor rhyolites as a late-stage feature along the continental margin. The basaltic magmas show a wide diversity in trace element and isotope composition, and a revised scheme of distinct magma types is proposed, based on new geochemical data plus a review of literature analyses, which retains the previously established overall classification i

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Pasa, Vaniza. "Estudo da conexão entre as drenagens do Médio Paraíba do Sul e do Alto Tietê: o caso do cotovelo de Guararema - SP, Brasil." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/8/8135/tde-23102013-125132/.

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Este trabalho trata da caracterização regional entre as drenagens dos rios Paraíba do Sul e Tietê, associada ao processo de captura fluvial, situado entre os municípios de Guararema e Mogi das Cruzes, no Estado de São Paulo. Parte-se da hipótese de processo de captura fluvial no médio curso do Paraíba do Sul e formação do cotovelo de Guararema, o que caracteriza essa anomalia como uma das mais interessantes do planeta Terra. É comum na região o padrão dendrítico e adensamento de drenagens cortados por falhas e fraturas de diversas idades. O embasamento é composto de estruturas cristalinas reco

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Mendes, Laura Delgado. "Termocronologia (U-Th)He e reativação da margem continental do sudeste do Brasil: seção Serra da Mantiqueira - Gráben da Guanabara." Universidade do Estado do Rio de Janeiro, 2013. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=7406.

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A evolução da margem continental do sudeste do Brasil tem sido discutida por diversos autores desde meados do século passado até os dias atuais, especialmente no contexto da origem e evolução dos escarpamentos e das bacias tafrogênicas. Buscou-se contribuir com novos dados sobre a evolução da área a partir da aplicação da termocronologia de baixa temperatura (U-Th)/He em apatita, que oferece uma sensibilidade significativa para registrar movimentações tectônicas na crosta superior. Foi possível obter idades em 107 cristais de apatita de 18 amostras do embasamento coletadas no perfil com orient

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Santos, Pedro Paulo Guy Martins dos. "Influência do campo de ventos e do meandramento da Corrente do Brasil na concentração de clorofila-a e nutrientes ao largo de Ubatuba - SP." Universidade de São Paulo, 2015. http://www.teses.usp.br/teses/disponiveis/21/21134/tde-23032016-145740/.

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O presente trabalho teve por objetivo estudar o efeito do campo de ventos e do meandramento da Corrente do Brasil nas variabilidades hidrográfica e bioquímica ao largo da costa norte do Estado de São Paulo. Foram utilizados dados de temperatura, nutrientes e clorofila-a obtidos in situ mensalmente ao largo de Ubatuba entre dezembro de 2004 a abril de 2014, dados do campo de ventos do pacote Blended Sea Winds (NCDC/NOAA), além de Temperatura da Superfície do Mar e Clorofila-a da Superfície do Mar do sensor MODIS/AQUA. Os dados obtidos mostraram que na primavera o vento paralelo teve forte corre

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Buchteile zum Thema "Continental Rift of Southern Brazil"

Gordon, Andres, Nivaldo Destro, and Monica Heilbron. "The Recôncavo-Tucano-Jatobá Rift and Associated Atlantic Continental Margin Basins." In São Francisco Craton, Eastern Brazil. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-01715-0_9.

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Wu, Zhengwen. "Shallow structure of the southern Albuquerque Basin (Rio Grande rift), New Mexico from COCORP seismic reflection data." In Reflection Seismology: The Continental Crust. American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd014p0293.

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Mello, Gilberto A., Roger D. Flood, Thomas H. Orsi, and Allen Lowrie. "Southern Brazil Basin: Sedimentary Processes and Features and Implications for Continental-Rise Evolution." In Geologic Evolution of Atlantic Continental Rises. Springer US, 1992. http://dx.doi.org/10.1007/978-1-4684-6500-6_8.

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Picarelli, Andre, and Vitor Abreu. "Sequence Stratigraphy Applied to Continental Rift BasinsExample from Recôncavo Basin, Brazil." In Lacustrine Sandstone Reservoirs and Hydrocarbon Systems. American Association of Petroleum Geologists, 2012. http://dx.doi.org/10.1306/13291396m953453.

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HUTCHINSON, D. R., and K. D. KLITGORD. "Evolution of rift basins on the continental margin off southern New England." In Developments in Geotectonics. Elsevier, 1988. http://dx.doi.org/10.1016/b978-0-444-42903-2.50009-9.

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Pindell, James, Rod Graham, Paul Bellingham, et al. "Continental Margin Formation and Creation of "Lateral Tectonic Accommodation Space" for Salt Deposition, Campos and Santos Basins, São Paulo Plateau, Brazil." In Petroleum Systems in "Rift" Basins. Gulf Coast Section SEPM, 2015. http://dx.doi.org/10.5724/gcs.15.34.0787.

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Love, F. R., and D. J. Stewart. "Exploration Using a Linked System Approach to the Rift and Drift Sections in Brazil." In Petroleum Systems of Divergent Continental Margin Basins: 25th Annual. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2005. http://dx.doi.org/10.5724/gcs.05.25.0768.

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MACK, GREG H., MIKE LEEDER, and STEPHEN L. SALYARDS. "TEMPORAL AND SPATIAL VARIABILITY OF ALLUVIAL-FAN AND AXIAL-FLUVIAL SEDIMENTATION IN THE PLIO-PLEISTOCENE PALOMAS HALF GRABEN, SOUTHERN RIO GRANDE RIFT, NEW MEXICO, U.S.A." In Sedimentation in Continental Rifts. SEPM (Society for Sedimentary Geology), 2002. http://dx.doi.org/10.2110/pec.02.73.0165.

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Ryan, Damien, Chris Boreham, Andrew Krassay, Ian Deighton, and Donna Cathro. "Systems of the Otway Basin, Southern Australia: Oil and Gas in a Complex Multi-Phase Rift Basin." In Petroleum Systems of Divergent Continental Margin Basins: 25th Annual. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2005. http://dx.doi.org/10.5724/gcs.05.25.0918.

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Potts, Richard, and Daniel Cole. "The Role of GIS in the Interdisciplinary Investigations at Olorgesailie, Kenya, a Pleistocene Archaeological Locality." In Anthropology, Space, and Geographic Information Systems. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195085754.003.0015.

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A geographic information system is an ideal tool for use in interdisciplinary studies because it provides automated means of linking and relating different spatial databases. In this paper we discuss GIS applications to ongoing archaeological and paleoecological studies at Olorgesailie, an early hominid archaeological locality in the rift valley of southern Kenya and one of the most noted Acheulian handaxe sites worldwide (Isaac 1977). The questions being asked in early hominid archaeology require thinking beyond individual artifacts and site excavations to broader spatial scales within welldefined time intervals (or chronostratigraphic units) (Blumenschine and Masao 1991; Potts 1991). The sedimentary exposures at Olorgesailie permit the smallest spatial scale of individual artifacts and fossils to be integrated with regional-scale studies. Since many of the GIS applications are still in initial form, the purpose here is largely to illustrate the conceptual framework by which GIS integrates the analysis of spatial data at varying geographic scales in the Olorgesailie basin. Covering over 4000 km in length, the African Rift System trends southward from the Afar Triangle in the Red Sea region to south of the Zambezi River in Zambia. The numerous continental rift basins that make up the rift system have a complex structural and volcanic history. For most of its length, the African Rift traverses Ethiopia, Kenya, and Tanzania. The rift is divisible into eastern and western portions, which merge into a broad faulted region in northern Tanzania (Baker et al. 1972). Between the eastern and western rifts, occupying portions of Uganda, Tanzania, and northern Kenya, is an uplifted plateau 1000 to 1200 m in elevation. Uplifted, elongated domal structures located in Ethiopia and Kenya form the structural base from which the East African Rift System has developed. The rocks that make up this shield complex are Precambrian gneisses, quartzites, and schists. In addition to intrusions by dikes and plutons, these basement rocks have been altered by partial melting and metamorphism. Significant though episodic uplift of the Kenyan dome and its flanks during the late Cretaceous and middle and late Tertiary contributed to the development of a graben structure (Baker 1986; Baker et al. 1972).

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Konferenzberichte zum Thema "Continental Rift of Southern Brazil"

Dunne, Jarrod, James Parsons, Daniel Maia, and Sergio Rogerio. "Explorational rock physics of post-rift sediments in the Southern Santos Basin, Brazil." In 15th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 31 July-3 August 2017. Brazilian Geophysical Society, 2017. http://dx.doi.org/10.1190/sbgf2017-005.

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Riva, Vinícius C. Dalla. "Paleodrainage mapping of the São Paulo southern continental shelf on the Santos basin." In 14th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 3-6 August 2015. Brazilian Geophysical Society, 2015. http://dx.doi.org/10.1190/sbgf2015-083.

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Corrêa, Thiago B. S., Cleverson G. Silva, and A. T. dos Reis. "Space-Time Evolution of the Marine Depocenters at the Pelotas Basin, Southern Brazilian Continental Margin." In 9th International Congress of the Brazilian Geophysical Society & EXPOGEF, Salvador, Bahia, Brazil, 11-14 September 2005. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2005. http://dx.doi.org/10.1190/sbgf2005-189.

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Clemens-Knott, Diane, Michelle L. Gevedon, Kalie M. Duccini, Rodrigo Aviles, Erin Boeshart, and Zoe Christine Kohler. "ENHANCED GEOCHRONOLOGIC RECORD OF SYN-RIFT PLUTONISM AND VOLCANISM IN THE JURASSIC CONTINENTAL MARGIN ARC, SOUTHERN SIERRA NEVADA MOUNTAINS (CA)." In 115th Annual GSA Cordilleran Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019cd-329649.

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Mepen, Michelle, Cleverson Guizan Silva, and Antonio Tadeu dos Reis. "Interaction of drift and gravitational depositional processes on the sedimentary architecture of the southern Brazilian continental margin." In 10th International Congress of the Brazilian Geophysical Society & EXPOGEF 2007, Rio de Janeiro, Brazil, 19-23 November 2007. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2007. http://dx.doi.org/10.1190/sbgf2007-448.

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Granath, James, and William Dickson. "Regionally Connected Structural Systems: The Power of the Big (Continental-Scale) Picture." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2571578-ms.

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ABSTRACT Beyond offshore West Africa where modern densely-sampled data from ships and satellites have played a key role in current understanding of passive margin evolution, Africa is in general rather unevenly known, especially in the subsurface in more remote areas. The GIS-based Exploration Fabric of Africa (EFA, the &lsquo;Purdy project&rsquo;) was designed to address that problem. It includes structural features such as faults and basin outlines but at a very high and often generalized level, divorced from their underlying genetic linkages. We have undertaken to compile a more det

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de Almeida, Anderson Gomes, Renato Oscar Kowsmann, and Alberto Garcia Figueiredo. "Quaternary submarine mass-transport complexes on the southern Continental Slope of Campos Basin characterized by AUV high frequency geophysical data." In 14th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 3-6 August 2015. Brazilian Geophysical Society, 2015. http://dx.doi.org/10.1190/sbgf2015-034.

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Sielski, Luiz Henrique, Rodolfo Jose Angulo, Maria Cristina Souza, and Fernando Alvim Veiga. "A low-cost approach to improve sediment mapping in shallow marine environment: A case study on the inner continental shelf of Parana, Southern Brazil." In 2017 IEEE/OES Acoustics in Underwater Geosciences Symposium (RIO Acoustics). IEEE, 2017. http://dx.doi.org/10.1109/rioacoustics.2017.8349745.

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de Almeida, Anderson Gomes, Renato Oscar Kowsmann, and Alberto Garcia Figueiredo. "P-wave velocity and Gamma density from multisensor core logger and its relation with deep-water sedimentary facies of Quaternary Mass-Transport Complex, Southern continental slope of Campos Basin." In 15th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 31 July-3 August 2017. Brazilian Geophysical Society, 2017. http://dx.doi.org/10.1190/sbgf2017-157.

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