Abstract
The Paramirim aulacogen is understood as an intracontinental rift system, nucleated around 1.75 Ga, in the central region of the São Francisco craton (SFC), which allowed the deposition of thick sedimentary sequences, predominantly siliciclastic and carbonate, such as the Espinhaço and São Francisco supergroups. The complex tectonic evolution of the CSF ultimately involved an intense proc…