Abstract
The southern Ribeira Belt is the result of an oblique collision between the São Francisco,Paranapanema and Luís Alves cratons, with the participation of microplates andallochthonous terrains remobilized during the Brasiliano-Pan-African cycle. This processresulted in a series of juxtaposed domains limited by shear zones that accumulatedappreciable horizontal displacements, some of which c…