The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene

Autores
Aragón, Eugenio; Aguilera, Emilia Yolanda; Cavarozzi, Claudia Ernestina; Ribot, Alejandro Mario; Rabassa, Jorge; Ollier, Cliff
Año de publicación
2014
Idioma
inglés
Tipo de recurso
parte de libro
Estado
versión publicada
Descripción
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.
Facultad de Ciencias Naturales y Museo
Materia
Geología
Altiplano
Patagonia
Plateau
Planation surface
Basalts
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/127383
Acceder
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oai_identifier_str oai:sedici.unlp.edu.ar:10915/127383
network_acronym_str SEDICI
repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the OligoceneAragón, EugenioAguilera, Emilia YolandaCavarozzi, Claudia ErnestinaRibot, Alejandro MarioRabassa, JorgeOllier, CliffGeologíaAltiplanoPatagoniaPlateauPlanation surfaceBasaltsThe 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.Facultad de Ciencias Naturales y MuseoSpringer, Dordrecht2014-02-22info:eu-repo/semantics/bookPartinfo:eu-repo/semantics/publishedVersionCapitulo de librohttp://purl.org/coar/resource_type/c_3248info:ar-repo/semantics/parteDeLibroapplication/pdf517-525http://sedici.unlp.edu.ar/handle/10915/127383enginfo:eu-repo/semantics/altIdentifier/isbn/978-94-007-7701-9info:eu-repo/semantics/altIdentifier/isbn/978-94-007-7702-6info:eu-repo/semantics/altIdentifier/doi/10.1007/978-94-007-7702-6_19info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-15T11:22:31Zoai:sedici.unlp.edu.ar:10915/127383Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-15 11:22:31.685SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
title The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
spellingShingle The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
Aragón, Eugenio
Geología
Altiplano
Patagonia
Plateau
Planation surface
Basalts
title_short The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
title_full The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
title_fullStr The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
title_full_unstemmed The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
title_sort The exhumation of the Northern Patagonian Massif Gondwana Planation surface due to uprising during the Oligocene
dc.creator.none.fl_str_mv Aragón, Eugenio
Aguilera, Emilia Yolanda
Cavarozzi, Claudia Ernestina
Ribot, Alejandro Mario
Rabassa, Jorge
Ollier, Cliff
author Aragón, Eugenio
author_facet Aragón, Eugenio
Aguilera, Emilia Yolanda
Cavarozzi, Claudia Ernestina
Ribot, Alejandro Mario
Rabassa, Jorge
Ollier, Cliff
author_role author
author2 Aguilera, Emilia Yolanda
Cavarozzi, Claudia Ernestina
Ribot, Alejandro Mario
Rabassa, Jorge
Ollier, Cliff
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Geología
Altiplano
Patagonia
Plateau
Planation surface
Basalts
topic Geología
Altiplano
Patagonia
Plateau
Planation surface
Basalts
dc.description.none.fl_txt_mv 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.
Facultad de Ciencias Naturales y Museo
description 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.
publishDate 2014
dc.date.none.fl_str_mv 2014-02-22
dc.type.none.fl_str_mv info:eu-repo/semantics/bookPart
info:eu-repo/semantics/publishedVersion
Capitulo de libro
http://purl.org/coar/resource_type/c_3248
info:ar-repo/semantics/parteDeLibro
format bookPart
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/127383
url http://sedici.unlp.edu.ar/handle/10915/127383
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/isbn/978-94-007-7701-9
info:eu-repo/semantics/altIdentifier/isbn/978-94-007-7702-6
info:eu-repo/semantics/altIdentifier/doi/10.1007/978-94-007-7702-6_19
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.format.none.fl_str_mv application/pdf
517-525
dc.publisher.none.fl_str_mv Springer, Dordrecht
publisher.none.fl_str_mv Springer, Dordrecht
dc.source.none.fl_str_mv reponame:SEDICI (UNLP)
instname:Universidad Nacional de La Plata
instacron:UNLP
reponame_str SEDICI (UNLP)
collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
instacron_str UNLP
institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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score 13.22299

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