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Osumilite-sapphirine-quartz granulites from Enderby Land, Antarctica: P-T conditions of metamorphism, implications for garnet-cordierite equilibria and the evolution of the deep crust

Earth ScienceDeep CrustEngineeringEnderby LandMetamorphic PetrologyGeologyCrustal MeltingGeochemistryOsumilite-sapphirine-quartz GranulitesMineral GeochemistryCrust-mantle InteractionPetrologyMetamorphic ProcessTectonics