“…During the Mesoneoproterozoic PanAfrican-Brazilian orogenic events (HEILBRON et al, 2000), the São Francisco Craton was part of the greater Late Upper Proterozoic São Francisco-Congo-Kalahari craton (HASUI, 2010), which is a Gondwanide continental block that originally extended east into South Africa and south into Antarctica (HASUI, 2010). With the Mesozoic break up (TROMPETTE et al, 1992), South America and Africa drifted apart in the Valanginian (LARSON; LADD, 1973; SIEDNER; MITCHEL, 1976), probably because of Cretaceous hot spots (ULBRICH; GOMES, 1981; THOMAZ FILHO; RODRIGUES, 1999; WHITE; MCKENZIE, 1989), which led to doming, uplift, as well as rifting processes and ultimately caused continental fragmentation (ALMEIDA 1976; SIEDNER; MITCHELL, 1976; COX, 1989).…”