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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/68464
Ver los metadatos del registro completo
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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 |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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13.13397 |