A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana

Autores
González, Pablo D.; Oriolo, Sebastián; Schulz, Bernhard; Naipauer, Maximiliano; Marcos, Paulo; Renda, Emiliano Manuel; Cábana, María Cecilia; Krause, Joachim
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The geologic evolution of the Gondwanide orogen recorded during the late Palaeozoic along thePanthalassan border of Gondwana is related to an active continental margin, though it is stilldebatable whether it was built by collision or accretion. To disentangle its orogenic processes andprovide constraints on the orogen type, we characterize the physicochemical conditions ofmetamorphism and associated deformation of the Mina Gonzalito Metamorphic Complex fromnorthern Patagonia (41°28’30” S-65°40’30” W). New field mapping and comprehensive petrochronologic analysis constrain the evolution of a thick-skinned fold and thrust belt in a retroarc setting, which is spatially and temporally related to the geometry and kinematics of the right-lateral reverse El Jagüelito ductile shear zone. Metamorphic evolution resulted in a clockwise P‐Tt-D path reflecting three stages of continuously changing P-T conditions under high-pressure(8.0–9.9 kbar) amphibolite facies (540–680°C) during a single-phase progressive ductile deformation event. Monazite ages ranging from 303 ± 5 to 252 ± 6 Ma account for the single-phase regional tectono-metamorphic event spanning ~ 50 My. Our results, integrated with regional data, led to interpreting the late Palaeozoic Gondwanide orogen developed along the Panthalassan margin of Gondwana as accretionary in advancing-mode.
Fil: González, Pablo D.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina
Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Schulz, Bernhard. Technische Universität Bergakademie Freiberg; Alemania
Fil: Naipauer, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina
Fil: Marcos, Paulo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Renda, Emiliano Manuel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Cábana, María Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Krause, Joachim. Helmholtz Institut Freiberg für Ressourcentechnologie; Alemania
Materia
GEOTHERMOBAROMETRY
PETROCHRONOLOGY
MONAZITE
LATE PALAEOZOIC
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
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oai:ri.conicet.gov.ar:11336/262735
Acceder
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network_acronym_str CONICETDig
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network_name_str CONICET Digital (CONICET)
spelling A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of GondwanaGonzález, Pablo D.Oriolo, SebastiánSchulz, BernhardNaipauer, MaximilianoMarcos, PauloRenda, Emiliano ManuelCábana, María CeciliaKrause, JoachimGEOTHERMOBAROMETRYPETROCHRONOLOGYMONAZITELATE PALAEOZOIChttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The geologic evolution of the Gondwanide orogen recorded during the late Palaeozoic along thePanthalassan border of Gondwana is related to an active continental margin, though it is stilldebatable whether it was built by collision or accretion. To disentangle its orogenic processes andprovide constraints on the orogen type, we characterize the physicochemical conditions ofmetamorphism and associated deformation of the Mina Gonzalito Metamorphic Complex fromnorthern Patagonia (41°28’30” S-65°40’30” W). New field mapping and comprehensive petrochronologic analysis constrain the evolution of a thick-skinned fold and thrust belt in a retroarc setting, which is spatially and temporally related to the geometry and kinematics of the right-lateral reverse El Jagüelito ductile shear zone. Metamorphic evolution resulted in a clockwise P‐Tt-D path reflecting three stages of continuously changing P-T conditions under high-pressure(8.0–9.9 kbar) amphibolite facies (540–680°C) during a single-phase progressive ductile deformation event. Monazite ages ranging from 303 ± 5 to 252 ± 6 Ma account for the single-phase regional tectono-metamorphic event spanning ~ 50 My. Our results, integrated with regional data, led to interpreting the late Palaeozoic Gondwanide orogen developed along the Panthalassan margin of Gondwana as accretionary in advancing-mode.Fil: González, Pablo D.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; ArgentinaFil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Schulz, Bernhard. Technische Universität Bergakademie Freiberg; AlemaniaFil: Naipauer, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; ArgentinaFil: Marcos, Paulo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; ArgentinaFil: Renda, Emiliano Manuel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; ArgentinaFil: Cábana, María Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; ArgentinaFil: Krause, Joachim. Helmholtz Institut Freiberg für Ressourcentechnologie; AlemaniaTaylor & Francis2024-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/262735González, Pablo D.; Oriolo, Sebastián; Schulz, Bernhard; Naipauer, Maximiliano; Marcos, Paulo; et al.; A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana; Taylor & Francis; International Geology Review; 67; 2; 7-2024; 125-1480020-6814CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/full/10.1080/00206814.2024.2375727info:eu-repo/semantics/altIdentifier/doi/10.1080/00206814.2024.2375727info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:35:03Zoai:ri.conicet.gov.ar:11336/262735instacron: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 09:35:03.579CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
title A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
spellingShingle A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
González, Pablo D.
GEOTHERMOBAROMETRY
PETROCHRONOLOGY
MONAZITE
LATE PALAEOZOIC
title_short A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
title_full A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
title_fullStr A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
title_full_unstemmed A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
title_sort A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana
dc.creator.none.fl_str_mv González, Pablo D.
Oriolo, Sebastián
Schulz, Bernhard
Naipauer, Maximiliano
Marcos, Paulo
Renda, Emiliano Manuel
Cábana, María Cecilia
Krause, Joachim
author González, Pablo D.
author_facet González, Pablo D.
Oriolo, Sebastián
Schulz, Bernhard
Naipauer, Maximiliano
Marcos, Paulo
Renda, Emiliano Manuel
Cábana, María Cecilia
Krause, Joachim
author_role author
author2 Oriolo, Sebastián
Schulz, Bernhard
Naipauer, Maximiliano
Marcos, Paulo
Renda, Emiliano Manuel
Cábana, María Cecilia
Krause, Joachim
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv GEOTHERMOBAROMETRY
PETROCHRONOLOGY
MONAZITE
LATE PALAEOZOIC
topic GEOTHERMOBAROMETRY
PETROCHRONOLOGY
MONAZITE
LATE PALAEOZOIC
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 geologic evolution of the Gondwanide orogen recorded during the late Palaeozoic along thePanthalassan border of Gondwana is related to an active continental margin, though it is stilldebatable whether it was built by collision or accretion. To disentangle its orogenic processes andprovide constraints on the orogen type, we characterize the physicochemical conditions ofmetamorphism and associated deformation of the Mina Gonzalito Metamorphic Complex fromnorthern Patagonia (41°28’30” S-65°40’30” W). New field mapping and comprehensive petrochronologic analysis constrain the evolution of a thick-skinned fold and thrust belt in a retroarc setting, which is spatially and temporally related to the geometry and kinematics of the right-lateral reverse El Jagüelito ductile shear zone. Metamorphic evolution resulted in a clockwise P‐Tt-D path reflecting three stages of continuously changing P-T conditions under high-pressure(8.0–9.9 kbar) amphibolite facies (540–680°C) during a single-phase progressive ductile deformation event. Monazite ages ranging from 303 ± 5 to 252 ± 6 Ma account for the single-phase regional tectono-metamorphic event spanning ~ 50 My. Our results, integrated with regional data, led to interpreting the late Palaeozoic Gondwanide orogen developed along the Panthalassan margin of Gondwana as accretionary in advancing-mode.
Fil: González, Pablo D.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina
Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Schulz, Bernhard. Technische Universität Bergakademie Freiberg; Alemania
Fil: Naipauer, Maximiliano. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina
Fil: Marcos, Paulo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Renda, Emiliano Manuel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Cábana, María Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Krause, Joachim. Helmholtz Institut Freiberg für Ressourcentechnologie; Alemania
description The geologic evolution of the Gondwanide orogen recorded during the late Palaeozoic along thePanthalassan border of Gondwana is related to an active continental margin, though it is stilldebatable whether it was built by collision or accretion. To disentangle its orogenic processes andprovide constraints on the orogen type, we characterize the physicochemical conditions ofmetamorphism and associated deformation of the Mina Gonzalito Metamorphic Complex fromnorthern Patagonia (41°28’30” S-65°40’30” W). New field mapping and comprehensive petrochronologic analysis constrain the evolution of a thick-skinned fold and thrust belt in a retroarc setting, which is spatially and temporally related to the geometry and kinematics of the right-lateral reverse El Jagüelito ductile shear zone. Metamorphic evolution resulted in a clockwise P‐Tt-D path reflecting three stages of continuously changing P-T conditions under high-pressure(8.0–9.9 kbar) amphibolite facies (540–680°C) during a single-phase progressive ductile deformation event. Monazite ages ranging from 303 ± 5 to 252 ± 6 Ma account for the single-phase regional tectono-metamorphic event spanning ~ 50 My. Our results, integrated with regional data, led to interpreting the late Palaeozoic Gondwanide orogen developed along the Panthalassan margin of Gondwana as accretionary in advancing-mode.
publishDate 2024
dc.date.none.fl_str_mv 2024-07
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/11336/262735
González, Pablo D.; Oriolo, Sebastián; Schulz, Bernhard; Naipauer, Maximiliano; Marcos, Paulo; et al.; A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana; Taylor & Francis; International Geology Review; 67; 2; 7-2024; 125-148
0020-6814
CONICET Digital
CONICET
url http://hdl.handle.net/11336/262735
identifier_str_mv González, Pablo D.; Oriolo, Sebastián; Schulz, Bernhard; Naipauer, Maximiliano; Marcos, Paulo; et al.; A clockwise P‐T‐t-D path of the northern Patagonia basement: implications for the Permian evolution of the Panthalassan margin of Gondwana; Taylor & Francis; International Geology Review; 67; 2; 7-2024; 125-148
0020-6814
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/full/10.1080/00206814.2024.2375727
info:eu-repo/semantics/altIdentifier/doi/10.1080/00206814.2024.2375727
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
application/pdf
dc.publisher.none.fl_str_mv Taylor & Francis
publisher.none.fl_str_mv Taylor & Francis
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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score 13.070432

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