Skip to main content

The Exhumation of the Northern Patagonian Massif Gondwana Planation Surface Due to Uprising During the Oligocene

  • Chapter
  • First Online:
Gondwana Landscapes in southern South America

Part of the book series: Springer Earth System Sciences ((SPRINGEREARTH))

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.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 169.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 219.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 219.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Similar content being viewed by others

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 Unpublished Doctoral Thesis, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina, 230 pp

    Google Scholar 

  • 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

    Article  Google Scholar 

  • 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

    Google Scholar 

  • 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

    Google Scholar 

  • 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

    Google Scholar 

  • 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

    Google Scholar 

  • 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

    Article  Google Scholar 

  • 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

    Google Scholar 

  • Cande SC, Leslie RB (1986) Late Cenozoic tectonics of the Southern Chile trench. J Geophys Res 91(B1):471–496

    Article  Google Scholar 

  • 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

    Google Scholar 

  • 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

    Google Scholar 

  • Corbella H (1984) El vulcanismo de la altiplanicie de Somuncura. In: 9º Congreso Geológico Argentino, Relatorio, 1, 10, 267–300

    Google Scholar 

  • Franchi MB, Nullo FE, Sepúlveda EG, Uliana MA (1984) Las sedimentitas Terciarias. In: 9º Congreso Geológico Argentino, Relatorio, 1, 9, 215–266

    Google Scholar 

  • 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

    Google Scholar 

  • González Díaz EF, Malagnino EC (1984) Geomorfología de la Provincia de Río Negro. In: 9º Congreso Geológico Argentino, Relatorio, 2, 1–159

    Google Scholar 

  • 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

    Google Scholar 

  • 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

    Google Scholar 

  • Rabassa J (1978) Paleorrelieves Cenozoicos en la región de Pilcaniyeu-Comallo, Provincia de Río Negro. In: 7º Congreso Geológico Argentino, Actas, 2, 77–87

    Google Scholar 

  • 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

    Google Scholar 

Download references

Acknowledgments

This research was supported by the following grants: CONICET PIP 00/916 and UNLP 11/534 and UNLP 11/689.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Eugenio Aragón .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2014 Springer Science+Business Media Dordrecht

About this chapter

Cite this chapter

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

Download citation

Publish with us

Policies and ethics