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Counterclockwise P–T path and isobaric cooling of metapelites from Brattnipene, Sør Rondane Mountains, East Antarctica: Implications for a tectonothermal event at the proto-Gondwana margin

Isobaric CoolingEngineeringContinental TectonicsMetamorphic PetrologyCounterclockwise P–t PathTectonic EvolutionGeologyCryospherePetrologyEarth ScienceProto-gondwana MarginTectonics