Neoarchean and Rhyacian TTG-Sanukitoid suites in the southern São Francisco Paleocontinent, Brazil: Evidence for diachronous change towards modern tectonics

Autor: Samuel Moreira Bersan, Mike Fowler, Henrique Bruno, Hugo Moreira, Claudio de Morisson Valeriano, Craig Storey, Rob Strachan, Luiz Guilherme do Eirado Silva, Ivo Dussin, Monica Heilbron, Julio Cesar Horta de Almeida, Carla Cristine Aguiar Neto, Miguel Tupinambá, Vitalino Elizeu

Publikováno v: Bruno, H, Elizeu, V, Heilbron, M, De Morisson Valeriano, C, Strachan, R, Fowler, M, Bersan, S, Moreira, H, Dussin, I, Guilherme Do Eirado Silva, L, Tupinambá, M, Almeida, J, Neto, C & Storey, C 2020, ' Neoarchean and Rhyacian TTG-Sanukitoid suites in the southern São Francisco Paleocontinent, Brazil: evidence for diachronous change towards modern tectonics ', Geoscience Frontiers . https://doi.org/10.1016/j.gsf.2020.01.015
Geoscience Frontiers, Vol 11, Iss 5, Pp 1763-1787 (2020)

The southern portion of the Sao Francisco Palaeocontinent in Brazil is denoted by Archean nuclei and Paleoproterozoic magmatic arcs that were amalgamated during Siderian to Orosirian orogenic processes (ca. 2.4–2.1 ​Ga). New isotopic U–Pb in zi

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https://doi.org/10.1016/j.gsf.2020.01.015