Abstract
The Southern Brasília Orogen is a record of convergence within the margins of the SãoFrancisco and Paranapanema paleoplates, recognized as a neoproterozoic subduction andcollision tectonic wedge located at the edge of the São Francisco Craton. From the Ediacaran(635Ma) it began to set up a system of nappes from high to ultra-high temperature and highpressure transported along the craton e…