The Vazante–Paracatu region represents the most important Zn district known in Brazil and
includes the Vazante hypogene non-sulfide Zn deposit composed mainly of willemite …

Paleoproterozoic to Mesoproterozoic cratonic basins in the São Francisco Craton are
classified into three megasequences: Statherian, Calymmian–early Ectasian, and Stenian …

The Neoproterozoic Brası́lia Belt, in central Brazil, includes in its eastern part a thick pile of
sediments deposited and deformed along the western margin of the São Francisco–Congo …

The Brasília belt is a well-preserved Neoproterozoic orogenic belt within the Tocantins
Province, central Brazil. Its northern segment strikes N–S, and verges eastwards to the São …

This chapter presents a review of the main tectonic features of the Southern Brasilia belt with
emphasis on its relationships with the southwestern margin of the São Francisco craton in …

O Grupo Paranoá corresponde a uma sucessão psamo-pelito-carbonatada depositada em
condições plataformais. A estratigrafia desse importante conjunto litoestratigráfico da Faixa …

Carbonate platforms were present worldwide during the Proterozoic Eon, and variations in
their C and Sr isotope ratios are commonly used as a correlation tool particularly through the …

The eastern portion of the Brasilia belt, part of the Neoproterozoic Tocantins Province in
central Brazil, is mainly constituted by metasedimentary rocks that partially represent the …

Understanding the delayed rise of eukaryotic life on Earth is one of the most fundamental
questions about biological evolution. Numerous studies have presented evidence for …

The São Francisco and the Congo cratons represent sectors of a Neoproterozoic
palaeocontinent preserved from the Brasiliano-Pan African orogeny, recorded in their …