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Insights into the origin of coexisting A1- and A2-type granites: Implications from zircon Hf-O isotopes of the Huayuangong intrusion in the Lower Yangtze River Belt, eastern China

EngineeringZircon Hf-o IsotopesTectonic EvolutionGeologyGeochemistryHuayuangong IntrusionGeochronologyA2-type GranitesOrogenyEarth ScienceTectonics