Paleozoic crustal blocks of onshore and offshore central Argentina: New pieces of the southwestern Gondwana collage and their role in the accretion of Patagonia and the evolution of Mesozoic south Atlantic sedimentary basins
The southwestern Gondwana basement block configuration in the central Argentinean offshore area was analyzed using gravimetric, magnetic and seismic data and existing onshore tectonic models. The resultant maps, the distribution of the Mesozoic and Cenozoic basins and Paleozoic structural features w...
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2012
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| LEADER | 30894caa a22018257a 4500 | ||
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| 001 | PAPER-23335 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205500.0 | ||
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| 024 | 7 | |2 scopus |a 2-s2.0-84864747691 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Páengaro, F. | |
| 245 | 1 | 0 | |a Paleozoic crustal blocks of onshore and offshore central Argentina: New pieces of the southwestern Gondwana collage and their role in the accretion of Patagonia and the evolution of Mesozoic south Atlantic sedimentary basins |
| 260 | |c 2012 | ||
| 270 | 1 | 0 | |m Páengaro, F.Av. República de Chile 330, 20031-170 Río de Janeiro, Brazil; email: francisco.pangaro@petrobras.com.br |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Tomezzoli, R.N., Vilas, J.F., Paleomagnetic constraints on the age of deformation of the Sierras Australes thrust and fold belt, Argentina (1999) Geophysical Journal Interior, 138, pp. 857-870 | ||
| 504 | |a Urien, C.M., Zambrano, J.J., Estructura del Margen Continental (1996) Geologia y recursos naturales de la plataforma continental Argentina, relatario XIII° Congreso Geologico Argentino y III° Congreso de Exploracion de Hidrocarboros, pp. 29-66. , Association Geologica Argentina & Inst. Argentino del Petroleo, Buenos Aires, Argentina, V.A. Ramos, M.A. Turic (Eds.) | ||
| 504 | |a Uriz, N., Cingolani, C., Chemale, F., Macambira, M., Armstrong, R., Isotopic studies on detrital zircons of Silurian-Devonian siliciclastic sequences from Argentinean North Patagonia and Sierra de la Ventana regions: comparative provenance (2011) International Journal of Earth Sciences (Geol Rundsch), 100, pp. 571-589 | ||
| 504 | |a Ventura Santos, R., Souza, P., Souza de Alvarenga, C.J., Dantas, E.L., Martins Pimentel, M., Gouveia de Oliveira, C., Medeiros de Araújo, L., Shrimp U-Pb zircon dating and palynology of bentonitic layers from the Permian Iratí formation, Paraná Basin, Brazil (2006) Gondwana Research, 9, pp. 456-463 | ||
| 504 | |a Veroslavsky, G., Daners, G., De Santa Ana, H., Rocas sedimentarias pérmicas en la plataforma continental uruguaya: el pre-rift de la Cuenca de Punta del Este (2003) Geogaceta, 34, pp. 203-206. , España | ||
| 504 | |a Veroslavsky, G., Ana, S., de, H., Rossello, E.A., Origen y evolución tectosedimentaria de los depósitos juroeocretácicos de la región meridional del Uruguay: su vinculación con el Lineamiento Santa Lucía-Aiguá-Merín (2004) Cuencas sedimentarias de Uruguay: Geología, paleontología y recursos minerales, pp. 117-142. , Ediciones DIRAC, Facultad de Ciencias, Universidad de la República, Montevideo, Uruguay, G. Veroslavsky, M. Ubilla, S. Martínez (Eds.) | ||
| 504 | |a von Gosen, W., Thrust tectonics in the North Patagonian massif (Argentina): implications for a Patagonian plate (2003) Tectonics, 22 (1). , 1005, 33 | ||
| 504 | |a Webster, R.E., Chebli, G.A., Fischer, J.F., General Levalle basin, Argentina: a frontier lower Cretaceous rift basin (2004) AAPG BULLETIN, pp. 627-652 | ||
| 504 | |a Werner, M., (2007), p. 425. , http://www.opus-bayern.de/uni-wuerzburg/volltexte/2007/2175/, The Stratigraphy, Sedimentology and Age of the Late Paleozoic Mesosaurus Inland Sea, SW Gondwana - New Implications from Studies on Sediments and Altered Pyroclastic Layers of the Dwyka and Ecca Group (Lower Karoo Supergroup) in Southern Namibia. Ph.D. thesis: Würzburg, University of Würzburg; Zalán, P.V., do Carmo, M., Severino, G., Rigoti, C.A., Magnavita, L.P., Oliveira, J.A.B., Viana, A.R., An Entirely New 3-D View of the Crustal and Mantle Structure of a South Atlantic Passive Margin - Santos, Campos and Espírito Santo Basins, Brazil (2011) AAPG Annual conference and Exhibition. April 10-13, 2011, , Texas, USA. Abstracts, Houston | ||
| 504 | |a Zambrano, J.J., Cuencas sedimentarias en el subsuelo de la provincia de Buenos Aires y zonas adyacentes (1974) Revista de la Asociación Geológica Argentina, 29, pp. 443-469 | ||
| 520 | 3 | |a The southwestern Gondwana basement block configuration in the central Argentinean offshore area was analyzed using gravimetric, magnetic and seismic data and existing onshore tectonic models. The resultant maps, the distribution of the Mesozoic and Cenozoic basins and Paleozoic structural features were used to validate the interpretations and to produce a new regional tectonic model. Pre-Carboniferous southwestern Gondwana of South America was interpreted as an open margin formed from east to west by the Dom Feliciano Belt, the Río de la Plata Craton, the Pampean Belt and the Pampia and Cuyania terranes. The collision of the Patagonia allochthonous terrane during the Late Paleozoic resulted in the development of the Ventania-Cape Fold Belt, which was mapped for the first time off the Argentinean coast out to 600 km from the shore. A strong change in the orientation of the Fold Belt is referred to as the Colorado Syntaxis, a mirror image of the Cape Syntaxis in South Africa. This change reflects the buttressing effect of the cratonic blocks that hamper the northward propagation of syncollisional deformation and resulted in a 180-km shift of the orogenic front. The Mesozoic basins and the basement block distribution were analyzed. The Pampean Belt, a deformed area produced by the Pampia accretion to the cratonic area, is the locus to two episutural basins, the General Levalle and Macachín basins. The Salado Basin was interpreted as an episutural basin controlled by a 2.1-2.0 Ga suture within the Rio de la Plata Craton. The Colorado Basin is composed of four segmented depocenters that reflect different emplacement controls: the location of the western Colorado Basin was controlled by the Upper Paleozoic orogen; the distributions of the central and eastern Colorado depocenters, orthogonal to the continental boundary, were also strongly influenced by the Upper Paleozoic structures and were offset by lineaments that reflect Dom Feliciano fabric; the Colorado Basin external depocenter that parallels the continental margin was also controlled by these lineaments. We interpret a time gap of some 50 Ma between the beginning of the evolution of the margin-orthogonal depocenters and the Atlantic breakup. © 2012 Elsevier Ltd. |l eng | |
| 593 | |a Petrobras de Argentina S.A. Exploration and Production, Argentina | ||
| 593 | |a IDEAN, Universidad de Buenos Aires, CONICET, Argentina | ||
| 690 | 1 | 0 | |a COLORADO BASIN |
| 690 | 1 | 0 | |a COLORADO SYNTAXIS |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a RIO DE LA PLATA CRATON |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a VENTANIA-CAPE FOLD BELT |
| 690 | 1 | 0 | |a COLORADO BASIN |
| 690 | 1 | 0 | |a COLORADO SYNTAXIS |
| 690 | 1 | 0 | |a FOLD BELTS |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a BUILDINGS |
| 690 | 1 | 0 | |a METAMORPHIC ROCKS |
| 690 | 1 | 0 | |a SEDIMENTARY ROCKS |
| 690 | 1 | 0 | |a TECTONICS |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a ACCRETION |
| 690 | 1 | 0 | |a ALLOCHTHON |
| 690 | 1 | 0 | |a BASEMENT ROCK |
| 690 | 1 | 0 | |a CONTINENTAL MARGIN |
| 690 | 1 | 0 | |a DEFORMATION |
| 690 | 1 | 0 | |a FOLD BELT |
| 690 | 1 | 0 | |a GONDWANA |
| 690 | 1 | 0 | |a GRAVIMETRY |
| 690 | 1 | 0 | |a LINEAMENT |
| 690 | 1 | 0 | |a MESOZOIC |
| 690 | 1 | 0 | |a PALEOZOIC |
| 690 | 1 | 0 | |a SEDIMENTARY BASIN |
| 690 | 1 | 0 | |a SEISMIC DATA |
| 690 | 1 | 0 | |a PATAGONIA |
| 700 | 1 | |a Ramos, V.A. | |
| 773 | 0 | |d 2012 |g v. 37 |h pp. 162-183 |k n. 1 |p Mar. Pet. Geol. |x 02648172 |t Marine and Petroleum Geology | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-84864747691&doi=10.1016%2fj.marpetgeo.2012.05.010&partnerID=40&md5=66ce1a37db490e71573d3adf731ea56d |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.marpetgeo.2012.05.010 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_02648172_v37_n1_p162_Paengaro |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02648172_v37_n1_p162_Paengaro |y Registro en la Biblioteca Digital |
| 961 | |a paper_02648172_v37_n1_p162_Paengaro |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 999 | |c 84288 | ||