Juréia - Itatins
Geological Evolution
This domain which is limited by the Cubatão and Itariri Shear Zones to the North / Northeast and the Serrinha Shear Zone to the South, constitutes the northeastern end of the Curitiba Terrane in the southern Ribeira Belt (Mantiqueira Province).
While the Neoproterozoic granites of the Juréia Massiv were formed about 750 million years ago during the collision of the Curitiba - and the Apiaí terrain in the course of the Brasiliano - Pan African cycle, crystallization times of more than 2 billion years indicate that the paleoproterozoic Itatins - granulites were formed during the fusion of the first (mirco-) continents on our planet (see also Atlantica) – Brazil / Travel & Tours.
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