Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
- Autores
- Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.
Fil: Toms, Phillip S.. University of London; Reino Unido
Fil: King, Matthew. University of London; Reino Unido
Fil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; Argentina
Fil: Kemp, Rob A.. University of London; Reino Unido
Fil: Foit Jr., Franklin F.. Washington State University; Estados Unidos - Materia
-
Alluvial Sequences
Argentina
Mendoza
Optical Dating
Tephrochronology - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/81803
Ver los metadatos del registro completo
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Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western ArgentinaToms, Phillip S.King, MatthewZárate, Marcelo ArístidesKemp, Rob A.Foit Jr., Franklin F.Alluvial SequencesArgentinaMendozaOptical DatingTephrochronologyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.Fil: Toms, Phillip S.. University of London; Reino UnidoFil: King, Matthew. University of London; Reino UnidoFil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; ArgentinaFil: Kemp, Rob A.. University of London; Reino UnidoFil: Foit Jr., Franklin F.. Washington State University; Estados UnidosAcademic Press Inc Elsevier Science2004-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/81803Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-750033-5894CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2004.05.005info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/geochemical-characterization-correlation-and-optical-dating-of-tephra-in-alluvial-sequences-of-central-western-argentina/A3A8DE4F94C415CCC7875125B9EDD55Ainfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:19:18Zoai:ri.conicet.gov.ar:11336/81803instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-10 13:19:18.32CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
title |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
spellingShingle |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina Toms, Phillip S. Alluvial Sequences Argentina Mendoza Optical Dating Tephrochronology |
title_short |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
title_full |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
title_fullStr |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
title_full_unstemmed |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
title_sort |
Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina |
dc.creator.none.fl_str_mv |
Toms, Phillip S. King, Matthew Zárate, Marcelo Arístides Kemp, Rob A. Foit Jr., Franklin F. |
author |
Toms, Phillip S. |
author_facet |
Toms, Phillip S. King, Matthew Zárate, Marcelo Arístides Kemp, Rob A. Foit Jr., Franklin F. |
author_role |
author |
author2 |
King, Matthew Zárate, Marcelo Arístides Kemp, Rob A. Foit Jr., Franklin F. |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Alluvial Sequences Argentina Mendoza Optical Dating Tephrochronology |
topic |
Alluvial Sequences Argentina Mendoza Optical Dating Tephrochronology |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study. Fil: Toms, Phillip S.. University of London; Reino Unido Fil: King, Matthew. University of London; Reino Unido Fil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; Argentina Fil: Kemp, Rob A.. University of London; Reino Unido Fil: Foit Jr., Franklin F.. Washington State University; Estados Unidos |
description |
The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study. |
publishDate |
2004 |
dc.date.none.fl_str_mv |
2004-07 |
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/11336/81803 Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-75 0033-5894 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/81803 |
identifier_str_mv |
Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-75 0033-5894 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2004.05.005 info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/geochemical-characterization-correlation-and-optical-dating-of-tephra-in-alluvial-sequences-of-central-western-argentina/A3A8DE4F94C415CCC7875125B9EDD55A |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Academic Press Inc Elsevier Science |
publisher.none.fl_str_mv |
Academic Press Inc Elsevier Science |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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12.48226 |