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Coeval TTG and sanukitoid magmatism during the Rhyacian tectonic evolution of the Juiz de Fora Complex (São Francisco Paleocontinent, SE-Brazil)
Transitioning tectonic regimes from stagnant lid to plate tectonic models is still challenging.
This tectonic transition appears to be diachronic in different old cratonic blocks worldwide …
This tectonic transition appears to be diachronic in different old cratonic blocks worldwide …