Landscape Evolution of Southern Patagonia

Autores
Schellmann, Gerhard; Wenzens, Gerd; Radtke, Ulrich; Trombotto, Dario Tomas; Zarate, Marcelo; Schnack, Enrique Jorge
Año de publicación
2000
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Investigations have been focused on the glacial history and valley development in the region of the terminal basins Lago Argentino, Lago Viedma and the adjacent Río Santa Cruz and Río Shehuen Valleys, as well as on the stratigraphic classification and absolute chronology of Middle and Late Quaternary coastal deposits along the Atlantic coast of Patagonia from the Península Valdés in the north to the Bay of San Julián in the south. They indicate that characteristics of Late Miocene and Early Pliocene times were the deposition of the widespread Patagonian Gravel formation and the main epirogenic uplifting, as well as the fluvial incision down to ca. 110 m above the recent valley floors, and that the oldest Andean foreland glaciations exntended to the east as fas as the major Pleistocene ones. Along the Patagonian Atlantic coast, which is characterized by a slow uplift trend, coastal terraces of Middle and Late Quaternary age are preserved in different elevations, probably as results of eustatic sea-level oscillations.
Fil: Schellmann, Gerhard. Universitat Essen; Alemania
Fil: Wenzens, Gerd. Universitat Dusseldorf; Alemania
Fil: Radtke, Ulrich. Universitat Zu Köln; Alemania
Fil: Trombotto, Dario Tomas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Zárate, Marcelo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Schnack, Enrique. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Laboratorio de Oceanografía Costera y Estuarios; Argentina
Materia
Glaciations
Souther Patagonia
Landscape
Esr
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/40897
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Landscape Evolution of Southern PatagoniaSchellmann, GerhardWenzens, GerdRadtke, UlrichTrombotto, Dario TomasZarate, MarceloSchnack, Enrique JorgeGlaciationsSouther PatagoniaLandscapeEsrhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Investigations have been focused on the glacial history and valley development in the region of the terminal basins Lago Argentino, Lago Viedma and the adjacent Río Santa Cruz and Río Shehuen Valleys, as well as on the stratigraphic classification and absolute chronology of Middle and Late Quaternary coastal deposits along the Atlantic coast of Patagonia from the Península Valdés in the north to the Bay of San Julián in the south. They indicate that characteristics of Late Miocene and Early Pliocene times were the deposition of the widespread Patagonian Gravel formation and the main epirogenic uplifting, as well as the fluvial incision down to ca. 110 m above the recent valley floors, and that the oldest Andean foreland glaciations exntended to the east as fas as the major Pleistocene ones. Along the Patagonian Atlantic coast, which is characterized by a slow uplift trend, coastal terraces of Middle and Late Quaternary age are preserved in different elevations, probably as results of eustatic sea-level oscillations.Fil: Schellmann, Gerhard. Universitat Essen; AlemaniaFil: Wenzens, Gerd. Universitat Dusseldorf; AlemaniaFil: Radtke, Ulrich. Universitat Zu Köln; AlemaniaFil: Trombotto, Dario Tomas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Zárate, Marcelo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Schnack, Enrique. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Laboratorio de Oceanografía Costera y Estuarios; ArgentinaE Schweizerbartsche Verlags2000-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/40897Schellmann, Gerhard; Wenzens, Gerd; Radtke, Ulrich; Trombotto, Dario Tomas; Zarate, Marcelo; et al.; Landscape Evolution of Southern Patagonia; E Schweizerbartsche Verlags; Zeitschrift für Angewandte Geologie; 1; 12-2000; 63-680044-2259CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.schweizerbart.de/publications/list/series/zaginfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:40:43Zoai:ri.conicet.gov.ar:11336/40897instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:40:44.227CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Landscape Evolution of Southern Patagonia
title Landscape Evolution of Southern Patagonia
spellingShingle Landscape Evolution of Southern Patagonia
Schellmann, Gerhard
Glaciations
Souther Patagonia
Landscape
Esr
title_short Landscape Evolution of Southern Patagonia
title_full Landscape Evolution of Southern Patagonia
title_fullStr Landscape Evolution of Southern Patagonia
title_full_unstemmed Landscape Evolution of Southern Patagonia
title_sort Landscape Evolution of Southern Patagonia
dc.creator.none.fl_str_mv Schellmann, Gerhard
Wenzens, Gerd
Radtke, Ulrich
Trombotto, Dario Tomas
Zarate, Marcelo
Schnack, Enrique Jorge
author Schellmann, Gerhard
author_facet Schellmann, Gerhard
Wenzens, Gerd
Radtke, Ulrich
Trombotto, Dario Tomas
Zarate, Marcelo
Schnack, Enrique Jorge
author_role author
author2 Wenzens, Gerd
Radtke, Ulrich
Trombotto, Dario Tomas
Zarate, Marcelo
Schnack, Enrique Jorge
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Glaciations
Souther Patagonia
Landscape
Esr
topic Glaciations
Souther Patagonia
Landscape
Esr
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Investigations have been focused on the glacial history and valley development in the region of the terminal basins Lago Argentino, Lago Viedma and the adjacent Río Santa Cruz and Río Shehuen Valleys, as well as on the stratigraphic classification and absolute chronology of Middle and Late Quaternary coastal deposits along the Atlantic coast of Patagonia from the Península Valdés in the north to the Bay of San Julián in the south. They indicate that characteristics of Late Miocene and Early Pliocene times were the deposition of the widespread Patagonian Gravel formation and the main epirogenic uplifting, as well as the fluvial incision down to ca. 110 m above the recent valley floors, and that the oldest Andean foreland glaciations exntended to the east as fas as the major Pleistocene ones. Along the Patagonian Atlantic coast, which is characterized by a slow uplift trend, coastal terraces of Middle and Late Quaternary age are preserved in different elevations, probably as results of eustatic sea-level oscillations.
Fil: Schellmann, Gerhard. Universitat Essen; Alemania
Fil: Wenzens, Gerd. Universitat Dusseldorf; Alemania
Fil: Radtke, Ulrich. Universitat Zu Köln; Alemania
Fil: Trombotto, Dario Tomas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Zárate, Marcelo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Schnack, Enrique. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Laboratorio de Oceanografía Costera y Estuarios; Argentina
description Investigations have been focused on the glacial history and valley development in the region of the terminal basins Lago Argentino, Lago Viedma and the adjacent Río Santa Cruz and Río Shehuen Valleys, as well as on the stratigraphic classification and absolute chronology of Middle and Late Quaternary coastal deposits along the Atlantic coast of Patagonia from the Península Valdés in the north to the Bay of San Julián in the south. They indicate that characteristics of Late Miocene and Early Pliocene times were the deposition of the widespread Patagonian Gravel formation and the main epirogenic uplifting, as well as the fluvial incision down to ca. 110 m above the recent valley floors, and that the oldest Andean foreland glaciations exntended to the east as fas as the major Pleistocene ones. Along the Patagonian Atlantic coast, which is characterized by a slow uplift trend, coastal terraces of Middle and Late Quaternary age are preserved in different elevations, probably as results of eustatic sea-level oscillations.
publishDate 2000
dc.date.none.fl_str_mv 2000-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/40897
Schellmann, Gerhard; Wenzens, Gerd; Radtke, Ulrich; Trombotto, Dario Tomas; Zarate, Marcelo; et al.; Landscape Evolution of Southern Patagonia; E Schweizerbartsche Verlags; Zeitschrift für Angewandte Geologie; 1; 12-2000; 63-68
0044-2259
CONICET Digital
CONICET
url http://hdl.handle.net/11336/40897
identifier_str_mv Schellmann, Gerhard; Wenzens, Gerd; Radtke, Ulrich; Trombotto, Dario Tomas; Zarate, Marcelo; et al.; Landscape Evolution of Southern Patagonia; E Schweizerbartsche Verlags; Zeitschrift für Angewandte Geologie; 1; 12-2000; 63-68
0044-2259
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.schweizerbart.de/publications/list/series/zag
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv E Schweizerbartsche Verlags
publisher.none.fl_str_mv E Schweizerbartsche Verlags
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1844613288691761152
score 13.070432

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