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Letter
Nature Geoscience 1, 321–323 (1 May 2008) | doi:10.1038/ngeo180
Partitioning of palladium at high pressures and temperatures during core formation
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Abstract
An early equilibration of the Earth|[rsquo]|s mantle with the metals that later formed the core may explain the concentrations of iron-loving (siderophile) elements in the mantle. However, a subset of these elements, the highly siderophile elements including palladium, are present in greater concentrations than expected.
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