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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/29449
Ver los metadatos del registro completo
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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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1844613876332625920 |
score |
13.070432 |