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Cogenetic silica-rich and carbonate-rich melts trapped in mantle minerals in Kerguelen ultramafic xenoliths: Implications for metasomatism in the oceanic upper mantle

Earth ScienceEngineeringIgneous PetrogenesisGeologyGeochemistryChemistryCarbonate-rich MeltsMantle MineralsKerguelen Ultramafic XenolithsPetrologyMantle Geochemistry