Skip navigation
Por favor, use este identificador para citar o enlazar este ítem: http://rid.unrn.edu.ar/handle/20.500.12049/11604

Registro completo de metadatos
Campo DC Valor Lengua/Idioma
dc.contributor.authorMarcos, Paulo-
dc.contributor.authorRenda, Emiliano Manuel-
dc.contributor.authorGonzález, Pablo Diego-
dc.contributor.authorOriolo, Sebastián-
dc.contributor.authorScivetti, Nicolás-
dc.contributor.authorBenedini, Leonardo-
dc.contributor.authorGeraldes, Mauro Cesar-
dc.contributor.authorGregori, Daniel-
dc.contributor.authorYoya, María Belén-
dc.contributor.authorBahía, Marcos Emanuel-
dc.date.accessioned2024-05-24T14:37:15Z-
dc.date.available2024-05-24T14:37:15Z-
dc.date.issued2024-05-13-
dc.identifier.otherhttps://proceedings.science/ssagi-2024/papers/lu-hf-zircon-analysis-as-a-discriminator-for-retreating-and-advancing-stages-in?lang=en-
dc.identifier.urihttp://rid.unrn.edu.ar/handle/20.500.12049/11604-
dc.language.isoenes_ES
dc.relation.urihttps://eventos.galoa.com.br/ssagi-2024/page/3287-homees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/-
dc.titleLu-Hf zircon analysis as a discriminator for retreating and advancing stages in accretionary orogens: A case study of Devonian to early Carboniferous igneous rocks in northwestern Patagoniaes_ES
dc.typeObjeto de conferenciaes_ES
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)-
dc.description.filiationMarcos, Paulo. Universidad Nacional de Río Negro (UNRN), Instituto de Investigación en Paleobiología y Geología (IIPG-CONICET), Río Negro, Argentina.es_ES
dc.description.filiationRenda, Emiliano Manuel. Universidad Nacional de Río Negro (UNRN), Instituto de Investigación en Paleobiología y Geología (IIPG-CONICET), Río Negro, Argentina.es_ES
dc.description.filiationGonzález, Pablo Diego. CONICET-SEGEMAR-UNRN. Río Negro, Argentina.es_ES
dc.description.filiationOriolo, Sebastián. Universidad de Buenos Aires (UBA). Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA-CONICET), Buenos Aires, Argentinaes_ES
dc.description.filiationScivetti, Nicolás. Instituto Patagónico de Geología y Paleontología (IPGP-CENPAT-CONICET), Chubut, Argentina.es_ES
dc.description.filiationBenedini, Leonardo. Universidad Nacional del Sur (UNS). Instituto Geológico del Sur (INGEOSUR). Buenos Aires, Argentina.es_ES
dc.description.filiationGeraldes, Mauro Cesar. Universidade do Estado do Rio de Janeiro. Rio do Janeiro, Brasil.es_ES
dc.description.filiationGregori, Daniel. Universidad Nacional del Sur (UNS). Instituto Geológico del Sur (INGEOSUR). Buenos Aires, Argentina.es_ES
dc.description.filiationYoya, María Belén. Universidad de Buenos Aires (UBA). Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires (IGEBA-CONICET), Buenos Aires, Argentinaes_ES
dc.description.filiationBahía, Marcos Emanuel. Universidad Nacional del Sur (UNS). Instituto Geológico del Sur (INGEOSUR). Buenos Aires, Argentina.es_ES
dc.subject.keywordLu-Hf zircon isotopeses_ES
dc.subject.keywordPaleozoic accretionary orogenes_ES
dc.subject.keywordRetreating and advancing stageses_ES
dc.subject.keywordNorthwestern Patagoniaes_ES
dc.type.versioninfo:eu-repo/semantics/acceptedVersiones_ES
dc.subject.materiaCiencias Exactas y Naturaleses_ES
dc.origin.lugarDesarrolloXIII South American Symposium on Isotope Geology. Búzios, Brasil.es_ES
dc.description.resumenThe geodynamic evolution of accretionary orogens is essentially ruled by variations in plate behavior, where a compressional upper plate stage defines advancing orogens, while an extensional upper plate stage characterizes retreating orogens (Cawood et al. 2009). Lu-Hf isotopes in igneous rocks have been demonstrated to be a sensitive system capable of distinguishing tectonic stage variations during orogenic growth (Marcos et al. 2023 and references therein). An advancing orogen stage produces magmatic rocks with negative εHf values linked to crustal melting processes resulting from the shortening and thickening of the continental crust. In contrast, a retreating orogen occurs when extensional settings prevail, leading to juvenile - mantle input that is detected by positive εHf values. Additionally, negative and positive εHf slopes across geological time allow for the identification of switches between these stages. The Terra Australis Orogen was an accretionary orogen that encompasses most of the Paleozoic rocks (~ 570 to 300 Ma) distributed along the eastern and western boundaries of Gondwana Supercontinent. The Devonian to early Carboniferous igneous-metamorphic basement is predominantly constrained along two basement segments in southern South America, marking the end of the Terra Australis Orogen. The northern segment is limited between 27° 30´ and 37° 30´ S, whereas the southern segment (39 - 43°S) comprises the oldest pre-Andean rocks in the northwestern Patagonian region. This study uses U-Th-Pb and Lu-Hf zircon isotopic coupling results to distinguish between compressional and extensional tectonic stages in the northwestern Patagonian basement. Contrasting settings with the northern segment are also summarized. The Devonian to Early Carboniferous igneous rocks in northwestern Patagonia could be divided into two main stages with extensional and compressional settings, respectively. The Early-Middle Devonian stage (~ 400 to 380 Ma) includes several isolated igneous and metaigneous outcrops that are widely distributed in the Patagonian Cordillera and surrounding regions. The εHf evolution from these rocks show progressive extensional conditions, transitioning from continental-arc magmatism with εHf values close to zero during early Devonian times (~ 400 to 390 Ma) to forearc and retroarc magmatism with positive εHf values during the early-middle Devonian (~ 395 to 385 Ma). The isotopic signature of the earliest stage suggests a significant juvenile magmatic source, particularly evident in forearc and retroarc regions. This pattern might be linked to an upper crust extensional stage characterized by the rise of the asthenospheric mantle through a thin continental crust. Deep subduction of the proto-Pacific plate is considered the most important tectonic factor triggering the retreating orogen phase (Marcos et al. 2023 and references therein). The second stage is characterized by a magmatic lull and the beginning of regional metamorphism during late Devonian – early Carboniferous times. Although positive εHf records persist in the forearc region, a negative εHf slope developed from the first to the second stage would evidence the beginning of a compressional stage. The transition from retreating to an advancing orogen configuration is possibly linked to a progressive shallowing of the proto-Pacific plate subduction reaching its climax during late Paleozoic times. A contrasting geodynamic evolution between the northern and southern segments of the Devonian to Early Carboniferous basement is distinguishable when comparing εHf data. The Devonian magmatism evolved within a compressive tectonic setting in the northern segment linked to negative εHf values and inboard magmatism migration, whereas the widespread Early Carboniferous magmatism could be attributed to an extensional phase triggered by a retreating orogen stage (Dahlquist et al. 2021).es_ES
dc.relation.journalTitleXIII South American Symposium on Isotope Geologyes_ES
dc.type.subtypeResumenes_ES
Aparece en las colecciones: Objetos de conferencia

Archivos en este ítem:
Archivo Descripción Tamaño Formato  
Marcos et al. (2024b) (XIII-SSAGI).pdf299,99 kBAdobe PDFVisualizar/Abrir
Mostrar el registro sencillo del ítem

Este documento es resultado del financiamiento otorgado por el Estado Nacional, por lo tanto queda sujeto al cumplimiento de la Ley N° 26.899


Este ítem está sujeto a una licencia Creative Commons Licencia Creative Commons Creative Commons