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Crystallisation ages in coeval silicic magma bodies: 238U–230Th disequilibrium evidence from the Rotoiti and Earthquake Flat eruption deposits, Taupo Volcanic Zone, New Zealand

Magmatic ProcessVolcanologyCrystallisation AgesEngineeringVolcanismNew ZealandGeologyTaupo Volcanic ZoneGeochemistryIgneous ProcessGeochronologyPetrologyEarth ScienceTectonics