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The generation of voluminous S-type granites in the Moldanubian unit, Bohemian Massif, by rapid isothermal exhumation of the metapelitic middle crust

Metamorphic ProcessMagmatic ProcessVolcanologyMetapelitic Middle CrustRapid Isothermal ExhumationEngineeringIgneous PetrogenesisMetamorphic PetrologyGeologyGeochemistryPetrologyEarth ScienceBohemian MassifTectonics