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Significant δ44/40Ca variations between carbonate- and clay-rich marine sediments from the Lesser Antilles forearc and implications for mantle heterogeneity

Marine GeologyEngineeringLesser Antilles ForearcIsotope GeochemistryMantle HeterogeneityGeologyGeochemistrySignificant δ44/40Ca VariationsEarth ScienceMantle GeochemistryTectonics