Basin fill evolution and paleotectonic patterns along the Samfrau geosyncline: The Sauce Grande basin-Ventana foldbelt (Argentina) and Karoo basin-Cape foldbelt (South Africa) revisited
As integral parts of du Toil's (1927) "Samfrau Geosyncline", the Sauce Grande basin-Ventana foldbelt (Argentina) and Karoo basin-Cape foldbelt (South Africa) share similar paleoclimatic, paleogeographic, and paleotectonic aspects related to the Late Paleozoic tectono-magmatic activity...
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1998
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| LEADER | 28953caa a22017417a 4500 | ||
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| 001 | PAPER-19728 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205106.0 | ||
| 008 | 190411s1998 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-54749084707 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a IJESF | ||
| 100 | 1 | |a López Gamundí, O.R. | |
| 245 | 1 | 0 | |a Basin fill evolution and paleotectonic patterns along the Samfrau geosyncline: The Sauce Grande basin-Ventana foldbelt (Argentina) and Karoo basin-Cape foldbelt (South Africa) revisited |
| 260 | |c 1998 | ||
| 270 | 1 | 0 | |m López Gamundí, O.R.; TEXACO Inc., International Exploration Division, 4800 Fournace Place, Bellaire, TX 77401-2324, United States; email: gamunor@texaco.com |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Visser, J.N.J., Sea-level changes in a back-arc-foreland transition: The late Carboniferous-Permian Karoo basin of South Africa (1993) Sediment Geol, 83, pp. 115-131 | ||
| 504 | |a Visser, J.N.J., Loock, J.C., Water depth in the main Karoo basin, South Africa, during Ecca (Permian) sedimentation (1978) Trans Geol Soc South Afr, 81, pp. 185-191 | ||
| 504 | |a Visser, J.N.J., Loock, J.C., Sedimentary facies of the Dwyka Formation associated with the Nooitgedacht glacial pavements, Barkly West District (1988) South Afr J Geol, 91, pp. 38-48 | ||
| 504 | |a Whateley, M.K.G., Deltaic and fluvial deposits of the Ecca group, Nongoma graben, northern Zululand (1980) Trans Geol Soc South Afr, 83, pp. 345-351 | ||
| 504 | |a De Wickens, H.V., Submarine fans of the Permian Ecca group in the SW Karroo basin: Their origin and reflection on the tectonic evolution of the basin and its source areas (1992) Inversion Tectonics of the Cape Fold Belt, Karroo and Cretaceous Basins of Southern Africa, pp. 117-126. , de Wit MJ, Ransome IGD (eds) Balkema, Rotterdam | ||
| 504 | |a De La Winter, H.R., Tectonostratigraphy, as applied to analysis of South African Phanerozoic basins (1984) Trans Geol Soc South Afr, 87, pp. 169-179 | ||
| 504 | |a De Wit, M.J., Ransome, I.G.D., Preliminary investigations into a microplate model for the South Western Cape (1992) Inversion Tectonics of the Cape Fold Belt, Karroo and Cretaceous Basins of Southern Africa, pp. 257-266. , de Wit MJ, Ransome IGD (eds) Balkema, Rotterdam | ||
| 504 | |a Zabala, C.A., Santiago, M.F., Amaolo, G.E., Depôsitos fluviales en la Formación Tunas (Pérmico). Cuenca paleozoica de Ventania. Provincia de Buenos Aires (1993) Revista Asociación Geológica Argentina, 48 (3-4), pp. 307-316 | ||
| 504 | |a Zalba, P.E., Morosi, M., Mineralogia de la bentonita pérmica de la Formación Yaguari, Uruguay (1990) Annual Meeting IUGS-IGCP Project 211 Late Paleozoic of South America, pp. 147-150. , Abstracts | ||
| 520 | 3 | |a As integral parts of du Toil's (1927) "Samfrau Geosyncline", the Sauce Grande basin-Ventana foldbelt (Argentina) and Karoo basin-Cape foldbelt (South Africa) share similar paleoclimatic, paleogeographic, and paleotectonic aspects related to the Late Paleozoic tectono-magmatic activity along the Panthalassan continental margin of Gondwanaland. Late Carboniferou-earliest Permian glacial deposits were deposited in the Sauce Grande (Sauce Grande Formation) and Karoo (Dwyka Formation) basins and Falkland-Malvinas Islands (Lafonia Formation) during an initial (sag) phase of extension. The pre-breakup position of the Falkland (Malvinas) Islands on the easternmost part of the Karoo basin (immediately east of the coast of South Africa) is supported by recent paleomagnetic data, lithofacies associations, paleoice flow directions and age similarities between the Dwyka and the Lafonia glacial sequences. The désintégration of the Gondwanan Ice Sheet (GIS) triggered widespread transgressions, reflected in the stratigraphie record by the presence of inter-basinally correctable, open marine, fine-grained deposits (Piedra Azul Formation in the Sauce Grande basin, Prince Albert Formation in the Karoo basin and Port Sussex Formation in the Falkland Islands) capping glacial marine sediments. These early postglacial transgressive deposits, characterised by fossils of the Eurydesma fauna and Glossopteris flora, represent the maximum flooding of the basins. Cratonward foreland subsidence was triggeredby the San Rafaël orogeny (ca. 270 Ma) in Argentina and propogated along the Gondwanan margin. This subsidence phase generated sufficient space to accommodate thick synorogenic sequences derived from the orogenic flanks of the Sauce Grande and Karoo basins. Compositionally, the initial extensional phase of these basins was characterized by quartz-rich, craton-derived detritus and was followed by a compressional (foreland) phase characterized by a paleocurrent reversal and dominance of arc/foldbelt-derived material. In the Sauce Grande basin, tuffs are interbedded in the upper half of the synorogenic, foldbelt-derived Tunas Formation (Early-early Late? Permian). Likewise, the first widespread appearance of tuffs in the Karoo basin is in the Whitehill Formation, of late Early Permian (260 Ma) age. Silicic volcanism along the Andes and Patagonia (Choiyoi magmatic province) peaked between the late Early Permian and Late Permian. A link between these volcanics and the consanguineous airborne tuffs present in the Sauce Grande and Karoo basins is suggested on the basis of their similar compositions and ages. © Springer-Verlag 1998. |l eng | |
| 593 | |a TEXACO Inc., International Exploration Division, 4800 Fournace Place, Bellaire, TX 77401-2324, United States | ||
| 593 | |a Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Ciudad Universitaria, Pabellôn 2, Buenos Aires 1428, Argentina | ||
| 690 | 1 | 0 | |a BASIN EVOLUTION |
| 690 | 1 | 0 | |a GONDWANALAND |
| 690 | 1 | 0 | |a KAROO BASIN |
| 690 | 1 | 0 | |a LATE PALEOZOIC |
| 690 | 1 | 0 | |a SAUCE GRANDE BASIN |
| 700 | 1 | |a Rossello, E.A. | |
| 773 | 0 | |d 1998 |g v. 86 |h pp. 819-834 |k n. 4 |p Int. J. Earth Sci. |x 14373254 |t International Journal of Earth Sciences | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-54749084707&partnerID=40&md5=eb8b1dc3c35292d1824d9f94c5ed3de4 |y Registro en Scopus |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_14373254_v86_n4_p819_LopezGamundi |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_14373254_v86_n4_p819_LopezGamundi |y Registro en la Biblioteca Digital |
| 961 | |a paper_14373254_v86_n4_p819_LopezGamundi |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 80681 | ||