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

Autores
González Díaz, E.F.; Folguera, A.
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
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.
Fuente
Rev. Asoc. Geol. Argent. 2011;68(1):17-32
Materia
drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/2.5/ar
Repositorio
Biblioteca Digital (UBA-FCEN)
Institución
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
OAI Identificador
paperaa:paper_00044822_v68_n1_p17_GonzalezDiaz
Acceder
id BDUBAFCEN_e4bcca333d057ae8e2494f159e8df87f
oai_identifier_str paperaa:paper_00044822_v68_n1_p17_GonzalezDiaz
network_acronym_str BDUBAFCEN
repository_id_str 1896
network_name_str Biblioteca Digital (UBA-FCEN)
spelling Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén González Díaz, E.F.Folguera, A.drainage basinfluvial processgeomorphologylandslidemorphogenesisstructural analysisArgentinaCordillera del VientoNeuquenTromen VolcanoThe 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.2011info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiazRev. Asoc. Geol. Argent. 2011;68(1):17-32reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2025-09-29T13:43:03Zpaperaa:paper_00044822_v68_n1_p17_GonzalezDiazInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-09-29 13:43:04.29Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse
dc.title.none.fl_str_mv Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
spellingShingle Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
González Díaz, E.F.
drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
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
dc.creator.none.fl_str_mv González Díaz, E.F.
Folguera, A.
author González Díaz, E.F.
author_facet González Díaz, E.F.
Folguera, A.
author_role author
author2 Folguera, A.
author2_role author
dc.subject.none.fl_str_mv drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
topic drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
dc.description.none.fl_txt_mv 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.
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.
publishDate 2011
dc.date.none.fl_str_mv 2011
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/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
url http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/2.5/ar
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv Rev. Asoc. Geol. Argent. 2011;68(1):17-32
reponame:Biblioteca Digital (UBA-FCEN)
instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron:UBA-FCEN
reponame_str Biblioteca Digital (UBA-FCEN)
collection Biblioteca Digital (UBA-FCEN)
instname_str Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron_str UBA-FCEN
institution UBA-FCEN
repository.name.fl_str_mv Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
repository.mail.fl_str_mv ana@bl.fcen.uba.ar
_version_ 1844618738108727296
score 13.070432

Publicaciones similares