Juvenile crust formed in the southern Brasília orogen basement at 2.08 and 2.15 Ga.
Geochemical signatures are subduction-related.
Felsic rocks with continental arc affinities predominate.
These are the southernmost and youngest recognized arcs related to the Mineiro Belt.
Part of a major continental crust generation event between 2.35 and 2.08 Ga.