New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina

Autores
Cingolani, Carlos Alberto; Uriz, Norberto Javier; Chemale Jr., Farid
Año de publicación
2010
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The geological evolution of Tandilia comprises mainly a juvenile igneous-metamorphic Paleoproterozoic basement named Buenos Aires Complex, which is covered by thin Neoproterozoic to Early Paleozoic sedimentary units which displays sub horizontal bedding (Fig. 1). This work is related to introduce the new detrital zircon U-Pb ages from two siliciclastic Neoproterozoic sequences called Villa Mónica and Cerro Negro Formations from the Barker region, and offer the comparison provenance analysis of these data with previous contributions in a paleogeographic interpretation.
Centro de Investigaciones Geológicas
Facultad de Ciencias Naturales y Museo
Materia
Geología
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/156756

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spelling New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, ArgentinaCingolani, Carlos AlbertoUriz, Norberto JavierChemale Jr., FaridGeologíaThe geological evolution of Tandilia comprises mainly a juvenile igneous-metamorphic Paleoproterozoic basement named Buenos Aires Complex, which is covered by thin Neoproterozoic to Early Paleozoic sedimentary units which displays sub horizontal bedding (Fig. 1). This work is related to introduce the new detrital zircon U-Pb ages from two siliciclastic Neoproterozoic sequences called Villa Mónica and Cerro Negro Formations from the Barker region, and offer the comparison provenance analysis of these data with previous contributions in a paleogeographic interpretation.Centro de Investigaciones GeológicasFacultad de Ciencias Naturales y Museo2010info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/156756enginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:40:46Zoai:sedici.unlp.edu.ar:10915/156756Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:40:47.061SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
title New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
spellingShingle New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
Cingolani, Carlos Alberto
Geología
title_short New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
title_full New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
title_fullStr New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
title_full_unstemmed New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
title_sort New detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
dc.creator.none.fl_str_mv Cingolani, Carlos Alberto
Uriz, Norberto Javier
Chemale Jr., Farid
author Cingolani, Carlos Alberto
author_facet Cingolani, Carlos Alberto
Uriz, Norberto Javier
Chemale Jr., Farid
author_role author
author2 Uriz, Norberto Javier
Chemale Jr., Farid
author2_role author
author
dc.subject.none.fl_str_mv Geología
topic Geología
dc.description.none.fl_txt_mv The geological evolution of Tandilia comprises mainly a juvenile igneous-metamorphic Paleoproterozoic basement named Buenos Aires Complex, which is covered by thin Neoproterozoic to Early Paleozoic sedimentary units which displays sub horizontal bedding (Fig. 1). This work is related to introduce the new detrital zircon U-Pb ages from two siliciclastic Neoproterozoic sequences called Villa Mónica and Cerro Negro Formations from the Barker region, and offer the comparison provenance analysis of these data with previous contributions in a paleogeographic interpretation.
Centro de Investigaciones Geológicas
Facultad de Ciencias Naturales y Museo
description The geological evolution of Tandilia comprises mainly a juvenile igneous-metamorphic Paleoproterozoic basement named Buenos Aires Complex, which is covered by thin Neoproterozoic to Early Paleozoic sedimentary units which displays sub horizontal bedding (Fig. 1). This work is related to introduce the new detrital zircon U-Pb ages from two siliciclastic Neoproterozoic sequences called Villa Mónica and Cerro Negro Formations from the Barker region, and offer the comparison provenance analysis of these data with previous contributions in a paleogeographic interpretation.
publishDate 2010
dc.date.none.fl_str_mv 2010
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info:eu-repo/semantics/publishedVersion
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url http://sedici.unlp.edu.ar/handle/10915/156756
dc.language.none.fl_str_mv eng
language eng
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