Isotopic U–Pb titanite and monazite data from the southern São Francisco craton better
constrain the timing of the tectono-thermal event that led to the amalgamation of the craton …

The Paleoproterozoic Transamazonian orogeny yielded a series of discrete orogens in
Brazil. The present field study in the Quadrilátero Ferrı́fero (QF) indicates that the southern …

In the last decade, the participation of the Amazonian Craton on Precambrian
supercontinents has been clarified thanks to a wealth of new paleomagnetic data. Paleo to …

The Congo (CC) and the São Francisco (SFC) cratons were joined at about 2.05 Ga;
northern parts of Palaeoproterozoic basement subsequently underwent extension at about 1 …

Recent geological, geochronological and isotopic studies allow the identification of four
important crustal segments in the basement of the São Francisco Craton in Bahia. The …

The Borborema Province of NE Brasil comprises the central part of a wide Pan-African-
Brasiliano orogenetic belt that formed as a consequence of late Neoproterozoic …

A mapping, tectonic (deformation, kinematics), petrologic (P–T paths) and geochronological
approach has enabled us to define the Paleoproterozoic West Central African Belt (WCAB) …

The reconstruction of a Palaeoproterozoic continental block requires correlation between
the major structural and lithological features of the main continental provinces. The African …

Recent geological, geochronological and isotopic research has identified four important
Archean crustal segments in the basement of the São Francisco Craton in the State of Bahia …

Abstract The Natividade-Cavalcanti crustal block is a Paleoproterozoic sialic terrain which
forms the basement of sedimentary sequences belonging to the Neoproterozoic Brasília Belt …