Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina

Autores
Mulcahy, Sean R.; Roeske, Sarah M.; McClelland, William C.; Ellis, Joshua R.; Jourdan, Fred; Renne, Paul R.; Vervoort, Jeffrey D.; Vujovich, Graciela Irene
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Famatina margin records an orogenic cycle of convergence, metamorphism, magmatism, and extension related to the accretion of the allochthonous Precordillera terrane. New structural, petrologic, and geochronologic data from the Loma de Las Chacras region demonstrate two distinct episodes of lower crustal migmatization. The first event preserves a counterclockwise pressure-temperature path in kyanite-K-feldspar pelitic migmatites that resulted in lower crustal migmatization via muscovite dehydration melting at ∼12 kbar and 868°C at 461 ±1.7 Ma. The shape of the pressure temperature path and timing of metamorphism are similar to those of regional midcrustal granulites and suggest pervasive Ordovician migmatization throughout the Famatina margin. One-dimensional thermal modeling coupled with regional isotopic data suggests Ordovician melts remained at temperatures above their solidus for 20–30 Ma following peak granulite facies metamorphism, throughout a time period marked by regional oblique convergence. The onset of synconvergent extension occurred only after regional migmatites cooled beneath their solidus and was synchronous with the cessation of Precordillera terrane accretion at ∼436 Ma. The second migmatite event was regionally localized and occurred at ∼700°C and 12 kbar between 411 and 407 Ma via vapor saturated melting of muscovite. Migmatization was synchronous with extension, exhumation, and strike-slip deformation that likely resulted from a change in the plate boundary configuration related to the convergence and collision of the Chilenia terrane.
Fil: Mulcahy, Sean R.. University of California at Berkeley; Estados Unidos
Fil: Roeske, Sarah M.. University of California at Davis; Estados Unidos
Fil: McClelland, William C.. University of Iowa; Estados Unidos
Fil: Ellis, Joshua R.. Kinross Gold Corporation; Canadá
Fil: Jourdan, Fred. Curtin University; Australia
Fil: Renne, Paul R.. University of California at Berkeley; Estados Unidos
Fil: Vervoort, Jeffrey D.. Washington State University; Estados Unidos
Fil: Vujovich, Graciela Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
OCLOYIC DEFORMATION
CHANIC DEFORMATION
CUYANIA
CHILENIA
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/29449

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network_name_str CONICET Digital (CONICET)
spelling Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest ArgentinaMulcahy, Sean R.Roeske, Sarah M.McClelland, William C.Ellis, Joshua R.Jourdan, FredRenne, Paul R.Vervoort, Jeffrey D.Vujovich, Graciela IreneOCLOYIC DEFORMATIONCHANIC DEFORMATIONCUYANIACHILENIAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Famatina margin records an orogenic cycle of convergence, metamorphism, magmatism, and extension related to the accretion of the allochthonous Precordillera terrane. New structural, petrologic, and geochronologic data from the Loma de Las Chacras region demonstrate two distinct episodes of lower crustal migmatization. The first event preserves a counterclockwise pressure-temperature path in kyanite-K-feldspar pelitic migmatites that resulted in lower crustal migmatization via muscovite dehydration melting at ∼12 kbar and 868°C at 461 ±1.7 Ma. The shape of the pressure temperature path and timing of metamorphism are similar to those of regional midcrustal granulites and suggest pervasive Ordovician migmatization throughout the Famatina margin. One-dimensional thermal modeling coupled with regional isotopic data suggests Ordovician melts remained at temperatures above their solidus for 20–30 Ma following peak granulite facies metamorphism, throughout a time period marked by regional oblique convergence. The onset of synconvergent extension occurred only after regional migmatites cooled beneath their solidus and was synchronous with the cessation of Precordillera terrane accretion at ∼436 Ma. The second migmatite event was regionally localized and occurred at ∼700°C and 12 kbar between 411 and 407 Ma via vapor saturated melting of muscovite. Migmatization was synchronous with extension, exhumation, and strike-slip deformation that likely resulted from a change in the plate boundary configuration related to the convergence and collision of the Chilenia terrane.Fil: Mulcahy, Sean R.. University of California at Berkeley; Estados UnidosFil: Roeske, Sarah M.. University of California at Davis; Estados UnidosFil: McClelland, William C.. University of Iowa; Estados UnidosFil: Ellis, Joshua R.. Kinross Gold Corporation; CanadáFil: Jourdan, Fred. Curtin University; AustraliaFil: Renne, Paul R.. University of California at Berkeley; Estados UnidosFil: Vervoort, Jeffrey D.. Washington State University; Estados UnidosFil: Vujovich, Graciela Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaAmerican Geophysical Union2014-04info: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/11336/29449Mulcahy, Sean R.; Roeske, Sarah M.; McClelland, William C.; Ellis, Joshua R.; Jourdan, Fred; et al.; Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina; American Geophysical Union; Tectonics; 33; 1; 4-2014; 1-250278-7407CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1002/2013TC003398info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2013TC003398/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:04:44Zoai:ri.conicet.gov.ar:11336/29449instacron: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:34982025-09-29 10:04:44.367CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
title Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
spellingShingle Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
Mulcahy, Sean R.
OCLOYIC DEFORMATION
CHANIC DEFORMATION
CUYANIA
CHILENIA
title_short Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
title_full Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
title_fullStr Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
title_full_unstemmed Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
title_sort Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina
dc.creator.none.fl_str_mv Mulcahy, Sean R.
Roeske, Sarah M.
McClelland, William C.
Ellis, Joshua R.
Jourdan, Fred
Renne, Paul R.
Vervoort, Jeffrey D.
Vujovich, Graciela Irene
author Mulcahy, Sean R.
author_facet Mulcahy, Sean R.
Roeske, Sarah M.
McClelland, William C.
Ellis, Joshua R.
Jourdan, Fred
Renne, Paul R.
Vervoort, Jeffrey D.
Vujovich, Graciela Irene
author_role author
author2 Roeske, Sarah M.
McClelland, William C.
Ellis, Joshua R.
Jourdan, Fred
Renne, Paul R.
Vervoort, Jeffrey D.
Vujovich, Graciela Irene
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv OCLOYIC DEFORMATION
CHANIC DEFORMATION
CUYANIA
CHILENIA
topic OCLOYIC DEFORMATION
CHANIC DEFORMATION
CUYANIA
CHILENIA
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 Famatina margin records an orogenic cycle of convergence, metamorphism, magmatism, and extension related to the accretion of the allochthonous Precordillera terrane. New structural, petrologic, and geochronologic data from the Loma de Las Chacras region demonstrate two distinct episodes of lower crustal migmatization. The first event preserves a counterclockwise pressure-temperature path in kyanite-K-feldspar pelitic migmatites that resulted in lower crustal migmatization via muscovite dehydration melting at ∼12 kbar and 868°C at 461 ±1.7 Ma. The shape of the pressure temperature path and timing of metamorphism are similar to those of regional midcrustal granulites and suggest pervasive Ordovician migmatization throughout the Famatina margin. One-dimensional thermal modeling coupled with regional isotopic data suggests Ordovician melts remained at temperatures above their solidus for 20–30 Ma following peak granulite facies metamorphism, throughout a time period marked by regional oblique convergence. The onset of synconvergent extension occurred only after regional migmatites cooled beneath their solidus and was synchronous with the cessation of Precordillera terrane accretion at ∼436 Ma. The second migmatite event was regionally localized and occurred at ∼700°C and 12 kbar between 411 and 407 Ma via vapor saturated melting of muscovite. Migmatization was synchronous with extension, exhumation, and strike-slip deformation that likely resulted from a change in the plate boundary configuration related to the convergence and collision of the Chilenia terrane.
Fil: Mulcahy, Sean R.. University of California at Berkeley; Estados Unidos
Fil: Roeske, Sarah M.. University of California at Davis; Estados Unidos
Fil: McClelland, William C.. University of Iowa; Estados Unidos
Fil: Ellis, Joshua R.. Kinross Gold Corporation; Canadá
Fil: Jourdan, Fred. Curtin University; Australia
Fil: Renne, Paul R.. University of California at Berkeley; Estados Unidos
Fil: Vervoort, Jeffrey D.. Washington State University; Estados Unidos
Fil: Vujovich, Graciela Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description The Famatina margin records an orogenic cycle of convergence, metamorphism, magmatism, and extension related to the accretion of the allochthonous Precordillera terrane. New structural, petrologic, and geochronologic data from the Loma de Las Chacras region demonstrate two distinct episodes of lower crustal migmatization. The first event preserves a counterclockwise pressure-temperature path in kyanite-K-feldspar pelitic migmatites that resulted in lower crustal migmatization via muscovite dehydration melting at ∼12 kbar and 868°C at 461 ±1.7 Ma. The shape of the pressure temperature path and timing of metamorphism are similar to those of regional midcrustal granulites and suggest pervasive Ordovician migmatization throughout the Famatina margin. One-dimensional thermal modeling coupled with regional isotopic data suggests Ordovician melts remained at temperatures above their solidus for 20–30 Ma following peak granulite facies metamorphism, throughout a time period marked by regional oblique convergence. The onset of synconvergent extension occurred only after regional migmatites cooled beneath their solidus and was synchronous with the cessation of Precordillera terrane accretion at ∼436 Ma. The second migmatite event was regionally localized and occurred at ∼700°C and 12 kbar between 411 and 407 Ma via vapor saturated melting of muscovite. Migmatization was synchronous with extension, exhumation, and strike-slip deformation that likely resulted from a change in the plate boundary configuration related to the convergence and collision of the Chilenia terrane.
publishDate 2014
dc.date.none.fl_str_mv 2014-04
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/11336/29449
Mulcahy, Sean R.; Roeske, Sarah M.; McClelland, William C.; Ellis, Joshua R.; Jourdan, Fred; et al.; Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina; American Geophysical Union; Tectonics; 33; 1; 4-2014; 1-25
0278-7407
CONICET Digital
CONICET
url http://hdl.handle.net/11336/29449
identifier_str_mv Mulcahy, Sean R.; Roeske, Sarah M.; McClelland, William C.; Ellis, Joshua R.; Jourdan, Fred; et al.; Multiple migmatite events and cooling from granulite facies metamorphism within the Famatina arc margin of northwest Argentina; American Geophysical Union; Tectonics; 33; 1; 4-2014; 1-25
0278-7407
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1002/2013TC003398
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/2013TC003398/abstract
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 American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection 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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