Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina

Autores
Mulcahy, S. R.; Roeske, S. M.; McClelland, W. C.; Jourdan, F.; Iriondo, A.; Renne, P. R.; Vervoort, J. D.; Vujovich, Graciela Irene
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks that were penetratively deformed during Ordovician accretion of the Precordillera terrane to the Gondwana margin. New structural, petrologic, and geochronologic data from a 40 km structural transect reveals that the Sierra de Pie de Palo preserves a middle to lower crustal ductile thrust complex consisting of individual structural units and not an intact ophiolite and cover sequence. Top-to-the-west thrusting occurred intermittently on discrete ductile shear zones from ∼515 to ∼417 Ma and generally propagated toward the foreland with progressive deformation. Ordovician crustal shortening and peak metamorphic temperatures in the central portion of the Sierra de Pie de Palo were synchronous with retro-arc shortening and magmatic flare-up within the Famatina arc. Accretion of the Precordillera terrane resulted in the end of arc flare-up and the onset of synconvergent extension by ∼439 Ma. Continued synextensional to postextensional convergence was accommodated along progressively lower grade shear zones following terrane accretion and the establishment of a new plate margin west of the Precordillera terrane. The results support models of Cordilleran orogens that link voluminous arc magmatism to periods of regional shortening. The deformation, metamorphic, and magmatic history within the Sierra de Pie de Palo is consistent with models placing the region adjacent to the Famatina margin in the middle Cambrian and not as basement to the Precordillera terrane.
Fil: Mulcahy, S. R.. University of Nevada; Estados Unidos. University of California at Davis; Estados Unidos
Fil: Roeske, S. M.. University of California at Davis; Estados Unidos
Fil: McClelland, W. C.. University of Iowa; Estados Unidos
Fil: Jourdan, F.. Curtin University; Australia. Berkeley Geochronology Center; Estados Unidos
Fil: Iriondo, A.. Universidad Nacional Autónoma de México; México
Fil: Renne, P. R.. Berkeley Geochronology Center; Estados Unidos. University of California at Berkeley; Estados Unidos
Fil: Vervoort, J. 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
STRUCTURE
GEOCHRONOLOGY
PIE DE PALO
CUYANIA / PRECORDILLERA TERRANE
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:11336/68464

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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest ArgentinaMulcahy, S. R.Roeske, S. M.McClelland, W. C.Jourdan, F.Iriondo, A.Renne, P. R.Vervoort, J. D.Vujovich, Graciela IreneSTRUCTUREGEOCHRONOLOGYPIE DE PALOCUYANIA / PRECORDILLERA TERRANEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks that were penetratively deformed during Ordovician accretion of the Precordillera terrane to the Gondwana margin. New structural, petrologic, and geochronologic data from a 40 km structural transect reveals that the Sierra de Pie de Palo preserves a middle to lower crustal ductile thrust complex consisting of individual structural units and not an intact ophiolite and cover sequence. Top-to-the-west thrusting occurred intermittently on discrete ductile shear zones from ∼515 to ∼417 Ma and generally propagated toward the foreland with progressive deformation. Ordovician crustal shortening and peak metamorphic temperatures in the central portion of the Sierra de Pie de Palo were synchronous with retro-arc shortening and magmatic flare-up within the Famatina arc. Accretion of the Precordillera terrane resulted in the end of arc flare-up and the onset of synconvergent extension by ∼439 Ma. Continued synextensional to postextensional convergence was accommodated along progressively lower grade shear zones following terrane accretion and the establishment of a new plate margin west of the Precordillera terrane. The results support models of Cordilleran orogens that link voluminous arc magmatism to periods of regional shortening. The deformation, metamorphic, and magmatic history within the Sierra de Pie de Palo is consistent with models placing the region adjacent to the Famatina margin in the middle Cambrian and not as basement to the Precordillera terrane.Fil: Mulcahy, S. R.. University of Nevada; Estados Unidos. University of California at Davis; Estados UnidosFil: Roeske, S. M.. University of California at Davis; Estados UnidosFil: McClelland, W. C.. University of Iowa; Estados UnidosFil: Jourdan, F.. Curtin University; Australia. Berkeley Geochronology Center; Estados UnidosFil: Iriondo, A.. Universidad Nacional Autónoma de México; MéxicoFil: Renne, P. R.. Berkeley Geochronology Center; Estados Unidos. University of California at Berkeley; Estados UnidosFil: Vervoort, J. 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 Union2011-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/68464Mulcahy, S. R.; Roeske, S. M.; McClelland, W. C.; Jourdan, F.; Iriondo, A.; et al.; Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina; American Geophysical Union; Tectonics; 30; 1; 2-2011; 1-250278-7407CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2009TC002656info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2009TC002656info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:46:43Zoai:ri.conicet.gov.ar:11336/68464instacron: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:34982025-09-03 09:46:44.016CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
title Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
spellingShingle Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
Mulcahy, S. R.
STRUCTURE
GEOCHRONOLOGY
PIE DE PALO
CUYANIA / PRECORDILLERA TERRANE
title_short Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
title_full Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
title_fullStr Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
title_full_unstemmed Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
title_sort Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina
dc.creator.none.fl_str_mv Mulcahy, S. R.
Roeske, S. M.
McClelland, W. C.
Jourdan, F.
Iriondo, A.
Renne, P. R.
Vervoort, J. D.
Vujovich, Graciela Irene
author Mulcahy, S. R.
author_facet Mulcahy, S. R.
Roeske, S. M.
McClelland, W. C.
Jourdan, F.
Iriondo, A.
Renne, P. R.
Vervoort, J. D.
Vujovich, Graciela Irene
author_role author
author2 Roeske, S. M.
McClelland, W. C.
Jourdan, F.
Iriondo, A.
Renne, P. R.
Vervoort, J. D.
Vujovich, Graciela Irene
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv STRUCTURE
GEOCHRONOLOGY
PIE DE PALO
CUYANIA / PRECORDILLERA TERRANE
topic STRUCTURE
GEOCHRONOLOGY
PIE DE PALO
CUYANIA / PRECORDILLERA TERRANE
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 Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks that were penetratively deformed during Ordovician accretion of the Precordillera terrane to the Gondwana margin. New structural, petrologic, and geochronologic data from a 40 km structural transect reveals that the Sierra de Pie de Palo preserves a middle to lower crustal ductile thrust complex consisting of individual structural units and not an intact ophiolite and cover sequence. Top-to-the-west thrusting occurred intermittently on discrete ductile shear zones from ∼515 to ∼417 Ma and generally propagated toward the foreland with progressive deformation. Ordovician crustal shortening and peak metamorphic temperatures in the central portion of the Sierra de Pie de Palo were synchronous with retro-arc shortening and magmatic flare-up within the Famatina arc. Accretion of the Precordillera terrane resulted in the end of arc flare-up and the onset of synconvergent extension by ∼439 Ma. Continued synextensional to postextensional convergence was accommodated along progressively lower grade shear zones following terrane accretion and the establishment of a new plate margin west of the Precordillera terrane. The results support models of Cordilleran orogens that link voluminous arc magmatism to periods of regional shortening. The deformation, metamorphic, and magmatic history within the Sierra de Pie de Palo is consistent with models placing the region adjacent to the Famatina margin in the middle Cambrian and not as basement to the Precordillera terrane.
Fil: Mulcahy, S. R.. University of Nevada; Estados Unidos. University of California at Davis; Estados Unidos
Fil: Roeske, S. M.. University of California at Davis; Estados Unidos
Fil: McClelland, W. C.. University of Iowa; Estados Unidos
Fil: Jourdan, F.. Curtin University; Australia. Berkeley Geochronology Center; Estados Unidos
Fil: Iriondo, A.. Universidad Nacional Autónoma de México; México
Fil: Renne, P. R.. Berkeley Geochronology Center; Estados Unidos. University of California at Berkeley; Estados Unidos
Fil: Vervoort, J. 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 Sierra de Pie de Palo of northwest Argentina preserves middle to lower crustal metamorphic rocks that were penetratively deformed during Ordovician accretion of the Precordillera terrane to the Gondwana margin. New structural, petrologic, and geochronologic data from a 40 km structural transect reveals that the Sierra de Pie de Palo preserves a middle to lower crustal ductile thrust complex consisting of individual structural units and not an intact ophiolite and cover sequence. Top-to-the-west thrusting occurred intermittently on discrete ductile shear zones from ∼515 to ∼417 Ma and generally propagated toward the foreland with progressive deformation. Ordovician crustal shortening and peak metamorphic temperatures in the central portion of the Sierra de Pie de Palo were synchronous with retro-arc shortening and magmatic flare-up within the Famatina arc. Accretion of the Precordillera terrane resulted in the end of arc flare-up and the onset of synconvergent extension by ∼439 Ma. Continued synextensional to postextensional convergence was accommodated along progressively lower grade shear zones following terrane accretion and the establishment of a new plate margin west of the Precordillera terrane. The results support models of Cordilleran orogens that link voluminous arc magmatism to periods of regional shortening. The deformation, metamorphic, and magmatic history within the Sierra de Pie de Palo is consistent with models placing the region adjacent to the Famatina margin in the middle Cambrian and not as basement to the Precordillera terrane.
publishDate 2011
dc.date.none.fl_str_mv 2011-02
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/11336/68464
Mulcahy, S. R.; Roeske, S. M.; McClelland, W. C.; Jourdan, F.; Iriondo, A.; et al.; Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina; American Geophysical Union; Tectonics; 30; 1; 2-2011; 1-25
0278-7407
CONICET Digital
CONICET
url http://hdl.handle.net/11336/68464
identifier_str_mv Mulcahy, S. R.; Roeske, S. M.; McClelland, W. C.; Jourdan, F.; Iriondo, A.; et al.; Structural evolution of a composite middle to lower crustal section: The Sierra de Pie de Palo, northwest Argentina; American Geophysical Union; Tectonics; 30; 1; 2-2011; 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/10.1029/2009TC002656
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2009TC002656
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 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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