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THE PRIMORDIAL CHONDRITIC NATURE AND LARGE-SCALE HETEROGENEITIES IN THE MANTLE - EVIDENCE FROM HIGH AND LOW PARTITION-COEFFICIENT ELEMENTS IN OCEANIC BASALTS
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MIXING IN NUMERICAL-MODELS OF MANTLE CONVECTION INCORPORATING PLATE KINEMATICS
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THE DESTRUCTION OF GEOCHEMICAL HETEROGENEITIES BY DIFFERENTIAL FLUID MOTIONS DURING MANTLE CONVECTION
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MIXING OF PASSIVE HETEROGENETIES BY MANTLE CONVECTION
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