Publication | Open Access

Post-collisional granitoids from the Dabie orogen: New evidence for partial melting of a thickened continental crust

Earth ScienceEngineeringContinental TectonicsNew EvidenceTectonic EvolutionGeologyCrustal MeltingGeochemistryPartial MeltingCrust-mantle InteractionOrogenyPetrologyDabie OrogenTectonics