A Paleoarchean (ca. 3.4 Ga) record from a TTG gneiss the São Francisco craton basement.
Early Mesoarchean (ca. 3.15 Ga) metamorphic overprinting on the Paleoarchean gneiss.
Siderian-Rhyacian-Orosirian links across the São Francisco craton basement.
Orosirian and Ediacaran overprinting on Archean and Paleoproterozoic former cratonic segments.