Reconstruction of a volcano-sedimentary environment shared by the Porongos and Várzea do Capivarita complexes at 790 Ma, Dom Feliciano Belt, southern Brazil

Author:

Battisti Matheus Ariel,Bitencourt Maria de Fátima,Schmitt Renata da Silva,Nardi Lauro Valentim Stoll,Martil Mariana Maturano Dias,De Toni Giuseppe Betino,Pimentel Márcio Martins,Armstrong Richard,Konopásek Jiří

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference99 articles.

1. U-Pb–Hf isotopes and trace elements of metasomatic zircon delimit the evolution of neoproterozoic Capané ophiolite in the southern Brasiliano Orogen;Arena;Int. Geol. Rev.,2018

2. The Dom Feliciano belt (Brazil-Uruguay)and its foreland (Rio de la Plata Craton): framework, tectonic evolution and correlations with similar terranes of southwestern Africa;Basei,2000

3. West Gondwana amalgamation based on detrital zircon ages from Neoproterozoic Ribeira and Dom Feliciano belts of South America and comparison with coeval sequences from SW Africa;Basei;Geol. Soc. London Spec. Publ.,2008

4. The basement of the Punta del Este Terrane (Uruguay): an African Mesoproterozoic fragment at the eastern border of the South American Río de La Plata craton;Basei;Int. J. Earth Sci.,2011

5. Evolução geológica (800–560 Ma) do setor central Do Cinturão Dom Feliciano com base no estudo petrológico, geocronológico e de proveniência dos complexos Porongos, Várzea Do Capivarita e Passo Feio, RS;Battisti,2022

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