Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite

This paper newly reports results of LA-ICPMS U-Pb dating for 282 zircon crystals separated from a Middle Miocene adakite in Cerro Pampa, southern Argentine Patagonia. With the exception of one spot age, 174 of the U-Pb concordia ages are markedly older (>94 Ma) than the cooling ages of the adakit...

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Autores: Orihashi, Yuji, Anma, Ryo, Motoki, Akihisa, Haller, Miguel Jorge F., Hirata, Daiji, Iwano, Hideki, Sumino, Hirochika, Ramos, Victor Alberto
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2013
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:inglés
OAI Identifier:oai:ri.conicet.gov.ar:11336/5400
Acceso en línea:http://hdl.handle.net/11336/5400
Access Level:acceso abierto
Palabra clave:Geochronological Fingerprint
Zircon
Adakite
La-Icpms
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
id AR_00a759387498a97c108116a338c5a878
oai_identifier_str oai:ri.conicet.gov.ar:11336/5400
network_acronym_str AR
network_name_str Argentina
repository_id_str
dc.title.none.fl_str_mv Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
title Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
spellingShingle Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
Orihashi, Yuji
Geochronological Fingerprint
Zircon
Adakite
La-Icpms
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
title_short Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
title_full Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
title_fullStr Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
title_full_unstemmed Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
title_sort Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite
dc.creator.none.fl_str_mv Orihashi, Yuji
Anma, Ryo
Motoki, Akihisa
Haller, Miguel Jorge F.
Hirata, Daiji
Iwano, Hideki
Sumino, Hirochika
Ramos, Victor Alberto
author Orihashi, Yuji
author_facet Orihashi, Yuji
Anma, Ryo
Motoki, Akihisa
Haller, Miguel Jorge F.
Hirata, Daiji
Iwano, Hideki
Sumino, Hirochika
Ramos, Victor Alberto
author_role author
author2 Anma, Ryo
Motoki, Akihisa
Haller, Miguel Jorge F.
Hirata, Daiji
Iwano, Hideki
Sumino, Hirochika
Ramos, Victor Alberto
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Geochronological Fingerprint
Zircon
Adakite
La-Icpms
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic Geochronological Fingerprint
Zircon
Adakite
La-Icpms
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description This paper newly reports results of LA-ICPMS U-Pb dating for 282 zircon crystals separated from a Middle Miocene adakite in Cerro Pampa, southern Argentine Patagonia. With the exception of one spot age, 174 of the U-Pb concordia ages are markedly older (>94 Ma) than the cooling ages of the adakite magma (ca. 12 Ma). The presence of numerous exotic zircon crystals indicates that the adakitic magma carries up information related to the crustal components during its ascent through the entire crust underneath Cerro Pampa. The obtained concordia ages of exotic zircons, 94-1335 Ma, are divisible into five groups having distinctive peaks on a population diagram. The first (94-125 Ma) and second age groups (125-145 Ma) correspond to the age of plutonic activities that formed the main body of the South Patagonian Batholith. The third to fifth groups respectively correspond to activities of the El Qumado-Ibañez volcanic complex (145-170 Ma), plutonic rocks scarcely exposed in Central Patagonia (170-200 Ma), and the Eastern Andean metamorphic complex of Late Paleozoic to Early Mesozoic ages (200-380 Ma). Our data suggest that the crust underneath Cerro Pampa was formed mostly after 380 Ma, the majority forming during the Early Cretaceous to Middle Jurassic. The processes of crustal development ceased for ca. 80 m.y. until the activity of the Cerro Pampa adakite in ca. 12 Ma. In contrast to the existence of numerous Archaean-Palaeoproterozoic exotic zircons in Mesozoic plutonic rocks distributed in Andean Cordillera at around 46°S, no evidence was found for Archaean-Paleoproterozoic crust on the Cerro Pampa region at 48°S. This evidence suggests that two crusts must have aggregated along a boundary between 46°S and 48°S with the continental margin of Gondwana during Late Paleozoic times, as part of the amalgamation of Pangea.
publishDate 2013
dc.date.none.fl_str_mv 2013-04
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/11336/5400
Orihashi, Yuji; Anma, Ryo; Motoki, Akihisa; Haller, Miguel Jorge F.; Hirata, Daiji; et al.; Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite; Geological Society of Japan; Geochemical Journal; 47; 2; 4-2013; 235-247
0016-7002
url http://hdl.handle.net/11336/5400
identifier_str_mv Orihashi, Yuji; Anma, Ryo; Motoki, Akihisa; Haller, Miguel Jorge F.; Hirata, Daiji; et al.; Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite; Geological Society of Japan; Geochemical Journal; 47; 2; 4-2013; 235-247
0016-7002
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.jstage.jst.go.jp/article/geochemj/47/2/47_2.0242/_article
info:eu-repo/semantics/altIdentifier/doi/
info:eu-repo/semantics/altIdentifier/url/http://doi.org/10.2343/geochemj.2.0242
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
application/pdf
dc.publisher.none.fl_str_mv Geological Society of Japan
publisher.none.fl_str_mv Geological Society of Japan
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
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
_version_ 1799195446820732928
spelling Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakiteOrihashi, YujiAnma, RyoMotoki, AkihisaHaller, Miguel Jorge F.Hirata, DaijiIwano, HidekiSumino, HirochikaRamos, Victor AlbertoGeochronological FingerprintZirconAdakiteLa-Icpmshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This paper newly reports results of LA-ICPMS U-Pb dating for 282 zircon crystals separated from a Middle Miocene adakite in Cerro Pampa, southern Argentine Patagonia. With the exception of one spot age, 174 of the U-Pb concordia ages are markedly older (>94 Ma) than the cooling ages of the adakite magma (ca. 12 Ma). The presence of numerous exotic zircon crystals indicates that the adakitic magma carries up information related to the crustal components during its ascent through the entire crust underneath Cerro Pampa. The obtained concordia ages of exotic zircons, 94-1335 Ma, are divisible into five groups having distinctive peaks on a population diagram. The first (94-125 Ma) and second age groups (125-145 Ma) correspond to the age of plutonic activities that formed the main body of the South Patagonian Batholith. The third to fifth groups respectively correspond to activities of the El Qumado-Ibañez volcanic complex (145-170 Ma), plutonic rocks scarcely exposed in Central Patagonia (170-200 Ma), and the Eastern Andean metamorphic complex of Late Paleozoic to Early Mesozoic ages (200-380 Ma). Our data suggest that the crust underneath Cerro Pampa was formed mostly after 380 Ma, the majority forming during the Early Cretaceous to Middle Jurassic. The processes of crustal development ceased for ca. 80 m.y. until the activity of the Cerro Pampa adakite in ca. 12 Ma. In contrast to the existence of numerous Archaean-Palaeoproterozoic exotic zircons in Mesozoic plutonic rocks distributed in Andean Cordillera at around 46°S, no evidence was found for Archaean-Paleoproterozoic crust on the Cerro Pampa region at 48°S. This evidence suggests that two crusts must have aggregated along a boundary between 46°S and 48°S with the continental margin of Gondwana during Late Paleozoic times, as part of the amalgamation of Pangea.Fil: Orihashi, Yuji. The University of Tokyo. Earthquake Research Institute; JapónFil: Anma, Ryo. University of Tsukuba. Graduate School of Life and Environmental Sciences; JapónFil: Motoki, Akihisa. Rio de Janeiro State University. Departamento de Mineralogia e Petrologia Ígnea; BrasilFil: Haller, Miguel Jorge F.. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico; ArgentinaFil: Hirata, Daiji. Kanagawa Prefecture Museum of Natural History; JapónFil: Iwano, Hideki. Kyoto Fission-Track; JapónFil: Sumino, Hirochika. University of Tokyo. Graduate School of Science. Geochemical Research Center; JapónFil: Ramos, Victor Alberto. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología. Laboratorio de Tectónica Andina; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos; ArgentinaGeological Society of Japan2013-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/5400Orihashi, Yuji; Anma, Ryo; Motoki, Akihisa; Haller, Miguel Jorge F.; Hirata, Daiji; et al.; Evolution history of the crust underlying Cerro Pampa, Argentine Patagonia: Constraint from LA-ICPMS U-Pb ages for exotic zircons in the Mid-Miocene adakite; Geological Society of Japan; Geochemical Journal; 47; 2; 4-2013; 235-2470016-7002enginfo:eu-repo/semantics/altIdentifier/url/https://www.jstage.jst.go.jp/article/geochemj/47/2/47_2.0242/_articleinfo:eu-repo/semantics/altIdentifier/doi/info:eu-repo/semantics/altIdentifier/url/http://doi.org/10.2343/geochemj.2.0242info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2024-05-08T13:52:47Zoai:ri.conicet.gov.ar:11336/5400instacron: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:34982024-05-08 13:52:48.105CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
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