title: Osmium-187 enrichment in some plumes: evidence for core-mantle interaction?
abstract: Calculations with data for asteroidal cores indicate that Earth's outer core may have a rhenium/osmium ratio at least 20 percent greater than that of the chondritic upper mantle, potentially leading to an outer core with an osmium-187/osmium-188 ratio at least 8 percent greater than that of chondrites. Because of the much greater abundance of osmium in the outer core relative to the mantle, even a small addition of metal to a plume ascending from the D" layer would transfer the enriched isotopic signature to the mixture. Sources of certain plume-derived systems seem to have osmium-187/osmium-l88 ratios 5 to 20 percent greater than that for chondrites, consistent with the ascent of a plume from the core-mantle boundary.
authors.forename: R J
authors.initials: RJ
authors.lastname: Walker
authors.forename: J W
authors.initials: JW
authors.lastname: Morgan
authors.forename: M F
authors.initials: MF
authors.lastname: Horan