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dc.date.accessioned 2021-09-20T13:18:35Z
dc.date.available 2021-09-20T13:18:35Z
dc.date.issued 2019
dc.identifier.uri http://sedici.unlp.edu.ar/handle/10915/125170
dc.description.abstract The “Lomagundi-Jatuli event” corresponds to the most important δ13C positive anomaly (≥5‰) globally reported in Palaeoproterozoic marine carbonates (between ∼2.30 and 2.06 Ga). In the Tandilia System (Argentina), Río de la Plata Craton, this event was recorded in the basement marble of the San Miguel area. The calcite-diopside marble, hosted by biotite gneiss and intruded by 2.12 Ga garnet-leucogranite, was metamorphosed in amphibolite facies during the Transamazonian Cycle. PAAS-normalised rare-earth elements (REE) and Y for the carbonate rocks are HREE-enriched and display positive Eu and Y anomalies, typical of primary precipitates from a mixed hydrothermal-marine environment carbonate. Additionally, a truly negative Ce anomaly for all the samples indicates that the depositional environment was oxidising. Positive δ13C values ranging from +5.90 to +4.30‰ (V-PDB), and δ18O from +17.45 to +13.84‰ (V-SMOW) were determined in this marble, both gradually decreasing towards the contact with the leucogranites. These values indicate that devolatilization reactions took place during the crystallisation of a wollastonite-vesuvianite-grossular-diopside skarn generated by the leucogranite intrusions into the marble. δ18O values obtained from diopside and calcite crystals, in the marble sectors furthest from the contacts with leucogranite, allowed a 663–623 °C formation temperature to be calculated, considering oxygen in a calcite-diopside geothermometric pair. These temperatures are consistent with the metamorphic degree (amphibolite facies) reached in this portion of the basement. Although the San Miguel marble shows petrographic and mineralogical evidence of regional and contact metamorphism, important geochemical and isotopic characteristics, together with its estimated Palaeoproterozoic age, indicate that the marble protolith was a marine carbonate deposited during the “Lomagundi-Jatuli event”. en
dc.format.extent 447-461 es
dc.language en es
dc.subject Lomagundi-Jatuli event es
dc.subject Carbon isotope es
dc.subject Metamorphism es
dc.subject Tandilia System es
dc.subject Palaeoproterozoic marble es
dc.title The Lomagundi-Jatuli carbon isotopic event recorded in the marble of the Tandilia System basement, Río de la Plata Craton, Argentina en
dc.type Articulo es
sedici.identifier.other doi:10.1016/j.precamres.2018.03.012 es
sedici.identifier.issn 0301-9268 es
sedici.creator.person Lajoinie, María Florencia es
sedici.creator.person Lanfranchini, Mabel Elena es
sedici.creator.person Recio, Clemente es
sedici.creator.person Sial, Alcides N. es
sedici.creator.person Cingolani, Carlos Alberto es
sedici.creator.person Ballivián Justiniano, Carlos Alberto es
sedici.creator.person Etcheverry, Ricardo Oscar es
sedici.subject.materias Geología es
sedici.description.fulltext true es
mods.originInfo.place Instituto de Recursos Minerales es
sedici.subtype Preprint es
sedici.rights.license Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
sedici.rights.uri http://creativecommons.org/licenses/by-nc-sa/4.0/
sedici.description.peerReview peer-review es
sedici.relation.journalTitle Precambrian Research es
sedici.relation.journalVolumeAndIssue vol. 326 es


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Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) Excepto donde se diga explícitamente, este item se publica bajo la siguiente licencia Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)