Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
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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Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai |
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I28-R145-paper_00044822_v68_n1_p17_GonzalezDiaz_oai2020-10-19 González Díaz, E.F. Folguera, A. 2011 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. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 2011;68(1):17-32 drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-145 |
collection |
Repositorio Digital de la Universidad de Buenos Aires (UBA) |
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 http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai |
work_keys_str_mv |
AT gonzalezdiazef geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen AT folgueraa geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen |
_version_ |
1766026493098459136 |