“…As discussed, a Paleozoic denudational cooling phase (Fig. 6) affected at least the SFC (Jelinek et al, 2014;Japsen et al, 2012 at the craton's continental margin) and Brasília Orogen (Fonseca et al, 2020). In the Matiqueira Province (Borba et al, 2002(Borba et al, , 2003Hueck et al, 2019;Machado et al, 2019;Oliveira et al, 2016;Ribeiro et al, 2005;Souza et al, 2014), Amazonian Craton (Harman et al, 1998) and ancient West Gondwana basement terrains in Africa (Kasanzu, 2017;Kasanzu et al, 2016), a Paleozoic cooling is also reported.…”