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History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29°–36° S revealed by a U–Pb and Lu–Hf isotope study of detrital zircon from late Paleozoic accretionary systems

South AmericaEngineeringPrecambrian GeologyGeographyCrustal GrowthTectonic EvolutionGeologyGeochemistryDetrital ZirconMesozoic TectonicsGeochronologyEarth ScienceTectonics