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Constraints on the sources of post-collisional K-rich magmatism: The roles of continental clastic sediments and terrigenous blueschists

Magmatic ProcessPost-collisional K-rich MagmatismVolcanologyEarth ScienceTerrigenous BlueschistsEngineeringContinental Clastic SedimentsMagmatismGeologyCrustal MeltingGeochemistryGeochronologyCrust-mantle InteractionPetrologyTectonics