dc.creatorCingolani, Carlos Alberto
dc.creatorUriz, Norberto Javier
dc.creatorChemale Jr., Farid
dc.date2010
dc.date2010
dc.date2023-08-23T18:23:42Z
dc.date.accessioned2024-07-24T03:42:25Z
dc.date.available2024-07-24T03:42:25Z
dc.identifierhttp://sedici.unlp.edu.ar/handle/10915/156756
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/9534930
dc.descriptionThe geological evolution of Tandilia comprises mainly a juvenile igneous-metamorphic Paleoproterozoic basement named Buenos Aires Complex, which is covered by thin Neoproterozoic to Early Paleozoic sedimentary units which displays sub horizontal bedding (Fig. 1). This work is related to introduce the new detrital zircon U-Pb ages from two siliciclastic Neoproterozoic sequences called Villa Mónica and Cerro Negro Formations from the Barker region, and offer the comparison provenance analysis of these data with previous contributions in a paleogeographic interpretation.
dc.descriptionCentro de Investigaciones Geológicas
dc.descriptionFacultad de Ciencias Naturales y Museo
dc.formatapplication/pdf
dc.languageen
dc.rightshttp://creativecommons.org/licenses/by-nc-sa/4.0/
dc.rightsCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.subjectGeología
dc.titleNew detrital zircon U-Pb ages on Neoproterozoic Tandilia sequences, Río de la Plata craton, Argentina
dc.typeObjeto de conferencia
dc.typeObjeto de conferencia


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