Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province

Autores
Mescua, J.F.; Giambiagi, L.B.; Bechis, F.
Año de publicación
2008
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
This contribution presents the results of a first stage of a study of the Tordillo Formation in southwestern Mendoza province. This unit, assigned to the Kimmeridgian, represents a continentalization of the Neuquén Basin. It consists mainly of fluvial deposits associated with eolian and playa lake deposits. The reconstruction of the thickness variations of this unit, the presence of synsedimentary normal faults and a provenance study in sandstones from two localities, which shows that sediment supply came from both margins of the basin, suggest that the Tordillo Formation was deposited during an extensional period, in a similar way to what is observed in the Cerro Aconcagua area and in the Sexta Region in Chile.
Fil:Mescua, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Giambiagi, L.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Bechis, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fuente
Rev. Asoc. Geol. Argent. 2008;63(4):512-519
Materia
Extension
Late Jurassic
Neuquén basin
Tordillo Formation
extensional tectonics
fluvial deposit
Jurassic
lacustrine deposit
normal fault
provenance
reconstruction
sandstone
synsedimentary tectonics
Argentina
Mendoza
Neuquen Basin
South America
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_v63_n4_p512_Mescua

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oai_identifier_str paperaa:paper_00044822_v63_n4_p512_Mescua
network_acronym_str BDUBAFCEN
repository_id_str 1896
network_name_str Biblioteca Digital (UBA-FCEN)
spelling Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province Mescua, J.F.Giambiagi, L.B.Bechis, F.ExtensionLate JurassicNeuquén basinTordillo Formationextensional tectonicsfluvial depositJurassiclacustrine depositnormal faultprovenancereconstructionsandstonesynsedimentary tectonicsArgentinaMendozaNeuquen BasinSouth AmericaThis contribution presents the results of a first stage of a study of the Tordillo Formation in southwestern Mendoza province. This unit, assigned to the Kimmeridgian, represents a continentalization of the Neuquén Basin. It consists mainly of fluvial deposits associated with eolian and playa lake deposits. The reconstruction of the thickness variations of this unit, the presence of synsedimentary normal faults and a provenance study in sandstones from two localities, which shows that sediment supply came from both margins of the basin, suggest that the Tordillo Formation was deposited during an extensional period, in a similar way to what is observed in the Cerro Aconcagua area and in the Sexta Region in Chile.Fil:Mescua, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Giambiagi, L.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Bechis, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.2008info: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_v63_n4_p512_MescuaRev. Asoc. Geol. Argent. 2008;63(4):512-519reponame: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/ar2025-11-27T08:36:51Zpaperaa:paper_00044822_v63_n4_p512_MescuaInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-11-27 08:36:52.837Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse
dc.title.none.fl_str_mv Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
title Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
spellingShingle Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
Mescua, J.F.
Extension
Late Jurassic
Neuquén basin
Tordillo Formation
extensional tectonics
fluvial deposit
Jurassic
lacustrine deposit
normal fault
provenance
reconstruction
sandstone
synsedimentary tectonics
Argentina
Mendoza
Neuquen Basin
South America
title_short Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
title_full Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
title_fullStr Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
title_full_unstemmed Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
title_sort Extensional tectonic evidences in the upper Jurassic (Kimmeridgian) in south-western Mendoza province
dc.creator.none.fl_str_mv Mescua, J.F.
Giambiagi, L.B.
Bechis, F.
author Mescua, J.F.
author_facet Mescua, J.F.
Giambiagi, L.B.
Bechis, F.
author_role author
author2 Giambiagi, L.B.
Bechis, F.
author2_role author
author
dc.subject.none.fl_str_mv Extension
Late Jurassic
Neuquén basin
Tordillo Formation
extensional tectonics
fluvial deposit
Jurassic
lacustrine deposit
normal fault
provenance
reconstruction
sandstone
synsedimentary tectonics
Argentina
Mendoza
Neuquen Basin
South America
topic Extension
Late Jurassic
Neuquén basin
Tordillo Formation
extensional tectonics
fluvial deposit
Jurassic
lacustrine deposit
normal fault
provenance
reconstruction
sandstone
synsedimentary tectonics
Argentina
Mendoza
Neuquen Basin
South America
dc.description.none.fl_txt_mv This contribution presents the results of a first stage of a study of the Tordillo Formation in southwestern Mendoza province. This unit, assigned to the Kimmeridgian, represents a continentalization of the Neuquén Basin. It consists mainly of fluvial deposits associated with eolian and playa lake deposits. The reconstruction of the thickness variations of this unit, the presence of synsedimentary normal faults and a provenance study in sandstones from two localities, which shows that sediment supply came from both margins of the basin, suggest that the Tordillo Formation was deposited during an extensional period, in a similar way to what is observed in the Cerro Aconcagua area and in the Sexta Region in Chile.
Fil:Mescua, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Giambiagi, L.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Bechis, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
description This contribution presents the results of a first stage of a study of the Tordillo Formation in southwestern Mendoza province. This unit, assigned to the Kimmeridgian, represents a continentalization of the Neuquén Basin. It consists mainly of fluvial deposits associated with eolian and playa lake deposits. The reconstruction of the thickness variations of this unit, the presence of synsedimentary normal faults and a provenance study in sandstones from two localities, which shows that sediment supply came from both margins of the basin, suggest that the Tordillo Formation was deposited during an extensional period, in a similar way to what is observed in the Cerro Aconcagua area and in the Sexta Region in Chile.
publishDate 2008
dc.date.none.fl_str_mv 2008
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_v63_n4_p512_Mescua
url http://hdl.handle.net/20.500.12110/paper_00044822_v63_n4_p512_Mescua
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. 2008;63(4):512-519
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
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score 13.011256