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Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root

Continental Arc RootMagmatic ProcessEarth ScienceEngineeringIgneous PetrogenesisGeologyCrustal MeltingGeochemistryCrust-mantle InteractionPost-collisional MeltingSveconorwegian Massif-type AnorthositesPetrologyTectonics