Abstract
The altiplano (or high plain) of the Northern Patagonian Massif is a large, 100,000 km2 geomorphological unit that rose from sea level to at least 1,200 metres above sea level (m a.s.l.) in Early Oligocene times, as a consequence of epeirogenic uplift. This uniform tableland feature is essentially a Cretaceous planation surface carved on Paleozoic igneous and metamorphic rocks of the Northern Patagonian Massif. This planation surface had been preserved by a thin and scattered cover of Maastrichtian-Danian marine sediments and Late Oligocene-Early Miocene basaltic flows. Erosion since Middle Miocene times at this tableland has exposed much of the Gondwana planation surface and developed numerous basaltic plateaus by relief inversion.
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References
Aguilera EY (2006) Identificación y distribución de distintas superficies geomorfológicas de escaso relieve local, por medio de sensores remotos en el área del Macizo Nordpatagónico, Provincia de Río Negro. Unpublished Doctoral Thesis, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina, 230 pp
Aragón E, González P, Aguilera EY, Cavarozzi C, Llambías E, Rivalenti G (2003) Thermal divide andesites-trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism. J S Am Earth Sci 16(3):91–103
Aragón E, Carroll AR, Aguilera EY, Cavarozzi C (2005) Ancient Gondwana landforms in Patagonia. In: Gondwana 12, “Geological and Biological Heritage of Gondwana”, Mendoza, Argentina, Abstracts, Academia Nacional de Ciencias, p 46
Aragón E, Aguilera EY, Cavarozzi C, Ubaldón MC, Ribot A (2008) La Caldera de Piedra Parada. Un volcán gigante de 50 millones de años, testimonio de cambios. In: Sitios de Interés Geológico, Ediciones Servicio Geológico Minero Argentino, Anales 46, 2, 669–682. Buenos Aires
Aragón E, Goin FJ, Aguilera EY, Woodburne MO, Carlini AA, Roggiero MF (2009) Paleogeography and paleoenvironments of Central Patagonia from the Late Cretaceous to the Miocene: the Paleogene Andean gap and the rise of the North Patagonian Altiplano, Abstracts, Workshop “Paleogeography and Paleoclimatology of Patagonia: effects on biodiversity”, Universidad Nacional de La Plata-Dalhousie University-CONICET-ANPCyT- National Science Foundation: PIRE (Partnerships for International Research & Education), La Plata
Aragón E, Aguilera EY, Cavarozzi C, Ribot A (2010) The North Patagonian Altiplano and the Somón Cura basaltic plateau. Geociências 29(4):527–532, São Paulo, UNESP, Brazil
Aragón E, Dèramo F, Brunelli D, Castro A, Rivalenti G, Varela R, Rabbia O, Spackman W, Cavarozzi CE, Aguilera EY, Mazzucchelli M, Demartis M-L, Ribot A (2011) Tectono-magmatic response to major convergence changes in the North Patagonian suprasubduction system: the Paleogene subduction-transcurrent plate margin transition. Tectonophysics 509:218–237
Ardolino A (1981) El volcanismo Cenozoico del borde suroccidental de la Meseta de Somún Curá. Provincia del Chubut. In: 8º Congreso Geológico Argentino, Actas, 3, 7–23
Cande SC, Leslie RB (1986) Late Cenozoic tectonics of the Southern Chile trench. J Geophys Res 91(B1):471–496
Cazau L, Mancini D, Cangini J, Spalletti L (1989) Cuenca Ñirihuau. In: Chebli G, Spalletti L (eds) Cuencas Sedimentarias de Argentina, Correlación Geológica 6, 299–318
Coira BL (1979) Descripción geológica de la hoja 40d, Ingeniero Jacobacci: provincia de Río Negro. Servicio Nacional Minero Geológico, Carta geológico-económica de la República Argentina. Escala 1:200.000, Argentina. Ministerio de Industria y Minería, Argentina. Subsecretaría de Minería, Boletín 168, 5–99. Buenos Aires
Corbella H (1984) El vulcanismo de la altiplanicie de Somuncura. In: 9º Congreso Geológico Argentino, Relatorio, 1, 10, 267–300
Franchi MB, Nullo FE, Sepúlveda EG, Uliana MA (1984) Las sedimentitas Terciarias. In: 9º Congreso Geológico Argentino, Relatorio, 1, 9, 215–266
González Bonorino F (1973) Geología de la región de San Carlos de Bariloche, provincia de Río Ngero. Fundación Bariloche, Publicaciones del Departamento de Recursos Naturales y Energía, San Carlos de Bariloche
González Díaz EF, Malagnino EC (1984) Geomorfología de la Provincia de Río Negro. In: 9º Congreso Geológico Argentino, Relatorio, 2, 1–159
Malumián N (1999) La sedimentación y el volcanismo Terciarios en la Patagonia extraandina. In: Caminos R (ed) Geología Argentina. Servicio Geológico Nacional, Anales 29, 18, 557–578, Buenos Aires
Nullo FE (1978) Descripción geológica de la hoja 41d, Lipetrén: provincia de Río Negro, Carta geológico-económica de la República Argentina. Escala 1:200.000, Argentina. Ministerio de Industria y Minería, Argentina. Subsecretaría de Minería, Servicio Nacional Minero Geológico, Boletín 158, 5–89. Buenos Aires
Rabassa J (1978) Paleorrelieves Cenozoicos en la región de Pilcaniyeu-Comallo, Provincia de Río Negro. In: 7º Congreso Geológico Argentino, Actas, 2, 77–87
Rapela CW, Spalletti L, Merodio JC, Aragón E (1987) Temporal evolution and spatial variation of the lower Tertiary Andean volcanism (40–42° 30′ S). J S Am Earth Sci 1:1–14
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This research was supported by the following grants: CONICET PIP 00/916 and UNLP 11/534 and UNLP 11/689.
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Aragón, E., Aguilera, E.Y., Cavarozzi, C.E., Ribot, A. (2014). The Exhumation of the Northern Patagonian Massif Gondwana Planation Surface Due to Uprising During the Oligocene. In: Rabassa, J., Ollier, C. (eds) Gondwana Landscapes in southern South America. Springer Earth System Sciences. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7702-6_19
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