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Strontium, neodymium, and lead isotope variations of authigenic and silicate sediment components from the Late Cenozoic Arctic Ocean: Implications for sediment provenance and the source of trace metals in seawater

Marine GeologyEngineeringTrace Element GeochemistryPaleoceanographyTrace MetalsIsotope GeochemistryLead Isotope VariationsMarine ChemistryGeologyOceanographyGeochemistrySediment ProvenanceGeochronologySedimentologyEarth Science