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Origin and evolution of multi-stage felsic melts in eastern Gangdese belt: Constraints from U–Pb zircon dating and Hf isotopic composition

Multi-stage Felsic MeltsEngineeringIgneous PetrogenesisU–pb Zircon DatingTectonic EvolutionGeologyCrustal MeltingGeochemistryGeochronologyPetrologyThermochronologyEarth ScienceEastern Gangdese BeltTectonics