Pd and Ag metal-silicate partitioning applied to Earth differentiation and core-mantle exchange

The lead isotopic age of the Earth can be explained by core formation alone

(2010) Bernard J. Wood et al.   NATURE

Core formation and metal–silicate fractionation of osmium and iridium from gold

(2009) James M. Brenan et al.   Nature Geoscience

Carbon solubility in core melts in a shallow magma ocean environment and distribution of carbon between the Earth’s core and the mantle

(2008) Rajdeep Dasgupta et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Silver isotope variations in chondrites: Volatile depletion and the initial 107Pd abundance of the solar system

(2008) M. Schönbächler et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Partitioning of palladium at high pressures and temperatures during core formation

(2008) K. Righter et al.   Nature Geoscience

Partitioning of molybdenum to 60 kbar along a warped Fe–FeS liquidus

(2007) David Walker et al.   CHEMICAL GEOLOGY