By Monica Heilbron,Umberto G. Cordani,Fernando F. Alkmim
Corresponding to the main intensively studied element of the Precambrian nucleus of the South American plate, the São Francisco craton and its margins host a rock list that spans from the Paleoarchean to the Cenozoic. Precambrian sedimentary successions that witness historical Earth techniques - a lot of them of worldwide importance - are specifically good preserved and uncovered during this quarter. With these kinds of attributes the São Francisco craton including its fringing orogenic belts will be considered as a ‘continent inside a continent’ or a ‘continent in miniature’.
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