Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén

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The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their varie...

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Autores principales:	González Díaz, E.F., Folguera, A.
Formato:	Artículo publishedVersion
Lenguaje:	Inglés
Publicado:	2011
Materias:	drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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spelling	paperaa:paper_00044822_v68_n1_p17_GonzalezDiaz2023-06-12T16:40:36Z Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén Rev. Asoc. Geol. Argent. 2011;68(1):17-32 González Díaz, E.F. Folguera, A. drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their variety and incidence through the time are expressed in the glacial morphogenesis concentrated in the western part of the Cordillera del Viento, in the volcanic landscape that predominates in the northern and eastern sectors (calderas, volcanoes, lava flows), in the structural control that defines the morphology of the fluvial process in the central zone and a firstly recognized important landslide to the north of Tricao Malal. As a result of the methodology employed two geological units of different age in the western part of the Tromen-Waile volcanic field were distinguished, which were initially interpreted as a single formation. A limited but consistent structural analysis of the region is also included. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2011 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion application/pdf eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
language	Inglés
orig_language_str_mv	eng
topic	drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano
spellingShingle	drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano González Díaz, E.F. Folguera, A. Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
topic_facet	drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano
description	The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their variety and incidence through the time are expressed in the glacial morphogenesis concentrated in the western part of the Cordillera del Viento, in the volcanic landscape that predominates in the northern and eastern sectors (calderas, volcanoes, lava flows), in the structural control that defines the morphology of the fluvial process in the central zone and a firstly recognized important landslide to the north of Tricao Malal. As a result of the methodology employed two geological units of different age in the western part of the Tromen-Waile volcanic field were distinguished, which were initially interpreted as a single formation. A limited but consistent structural analysis of the region is also included.
format	Artículo Artículo publishedVersion
author	González Díaz, E.F. Folguera, A.
author_facet	González Díaz, E.F. Folguera, A.
author_sort	González Díaz, E.F.
title	Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_short	Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_full	Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_fullStr	Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_full_unstemmed	Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_sort	geomorphologic analysis of the lower and middle section of the drainage basin of the curri leuvúriver, neuquén
publishDate	2011
url	http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
work_keys_str_mv	AT gonzalezdiazef geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen AT folgueraa geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen
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Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén

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