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Coupled Hf–Nd–Pb isotope co-variations of HIMU oceanic island basalts from Mangaia, Cook-Austral islands, suggest an Archean source component in the mantle transition zone

VolcanologyEngineeringArchean Source ComponentIgneous PetrogenesisIsotope GeochemistryCook-austral IslandsGeologyMantle Transition ZoneGeochemistryCrust-mantle InteractionEarth ScienceMantle GeochemistryTectonics