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Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbite

Carajás ProvinceEngineeringPrecambrian GeologyPium ComplexGeologyGeochemistryMesozoic TectonicsChemistryGeochronologyPetrologyComplex ZirconsTectonics