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dc.contributor.authorGreco, Gerson Alan-
dc.contributor.authorGonzález, Santiago Nicolás-
dc.contributor.authorGonzález, Pablo Diego-
dc.contributor.authorSato, Ana Maria-
dc.contributor.authorLlambías, Eduardo Jorge-
dc.contributor.authorColombo Celso, Gaeta Tassinari-
dc.contributor.authorStipp Basei, Miguel Angelo-
dc.contributor.authorSato, Kei-
dc.contributor.authorVarela, Ricardo-
dc.date.accessioned2020-08-31T15:27:46Z-
dc.date.available2020-08-31T15:27:46Z-
dc.date.issued2014-
dc.identifier.urihttp://rid.unrn.edu.ar/handle/20.500.12049/5683-
dc.language.isoenes_ES
dc.relation.ispartof9th South American Symposium on Isotope Geologyes_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/-
dc.titleCambrian magmatism and Cambro-Ordovician tectono-metamorphic event in Nahuel Niyeu Formation, Northpatagonian Massif, Argentinaes_ES
dc.typeObjeto de conferenciaes_ES
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)-
dc.description.filiationGreco, Gerson. Centro de Investigaciones Geológicas (UNLP-CONICET); Argentina.es_ES
dc.description.filiationGonzález, Santiago Nicolás. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.description.filiationGonzález, Pablo Diego. Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro, Argentina.es_ES
dc.description.filiationSato, Ana María. Centro de Investigaciones Geológicas (UNLP-CONICET); Argentina.es_ES
dc.description.filiationLlambías, Eduardo. Centro de Investigaciones Geológicas (UNLP-CONICET); Argentina.es_ES
dc.description.filiationColombo, Tassinari Celso. Universidade de Sao Paulo; Brasil.es_ES
dc.description.filiationBasei, Miguel. Centro de Investigaciones Geológicas (UNLP-CONICET); Argentina.es_ES
dc.description.filiationSato, Kei. Instituto de Geociencias; Brasil.es_ES
dc.description.filiationVarela, Ricardo. Centro de Investigaciones Geológicas (UNLP-CONICET); Argentina.es_ES
dc.subject.keywordCambrian Magmatismes_ES
dc.subject.keywordCambro Ordovicianmes_ES
dc.subject.keywordTectono Metamorphices_ES
dc.subject.keywordNahuel Niyeu Formationes_ES
dc.type.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.subject.materia.::Ciencias Exactas y Naturaleses_ES
dc.origin.lugarDesarrolloUniversidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología.es_ES
dc.description.resumenNahuel Niyeu Formation metasediments are interbedded with metamafic sills between Valcheta and Aguada Cecilio towns, Rio Negro Province, Argentina. The sills display clear intrusive contacts, concordant with relict, sedimentary S0 bedding. Their composition is dominantly gabbroic, with minor granodioritic and even granitic differentiates. A main tectono metamorphic event (D1-D2-M1) at greenschist facies affects both the sedimentary and interbedded igneous protoliths. Muscovite leucogranites, equivalent to the Valcheta Pluton of 470 Ma (Ar-Ar, Gozalvez 2009), and therefore of possible Ordovician age, crosscut the sills and metasediments in postorogenic relationship. Zircon crystals were collected from a granitic differentiate of a sill and analysed by SHRIMP U-Pb method at the Centro de Pesquisas Geocronologicas, Geosciences Institute, University of São Paulo. Cathodoluminescence (CL), Secondary Electron (SE), and binocular lens images were used for choosing the sites for analysis on the basis of internal structure and fracturing degree of the grains. The crystals are prismatic, amber colour or colourless and transparent, they present low luminescence and show oscillatory and sector zoning, typical of magmatic zircon. The U-Pb SHRIMP analysis yielded a Cambrian concordia age of 513.6 ± 3.3 Ma (MSWD = 0.84). This result is interpreted as the age of magmatic crystallization of the sill. From the above, a Cambrian magmatism (513.6 ± 3.3 Ma) of mainly basic composition is confirmed. This magmatism is coeval with the deposition of the sedimentary protoliths of the Nahuel Niyeu Formation, since their maximum deposition age is around 515-507 Ma (Pankhurst et al. 2006; Rapalini et al. 2013). Furthermore, the first and main tectono metamorphic event (D1-D2-M1) may be constrained between 513.6 and 470 Ma, on the basis of the equivalence of the postorogenic leucogranites with the 470 Ma, Valcheta Granite.es_ES
dc.type.subtypeResumenes_ES
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