![]() Laboratory partitioning of platinum-group elements (PGE) and gold with application to magmatic sulfide-PGE deposits. Geochimica et Cosmochimica Acta, 168, 151–171.įleet, M. Ru isotope heterogeneity in the solar protoplanetary disk. Rhodium, gold and other highly siderophile elements in orogenic peridotites and peridotite xenoliths. Negative thermal ion mass-spectrometry of osmium, rhenium, and iridium. Journal of Geophysical Research, 88(S2), A507–A518.Ĭreaser, R. Siderophile trace elements in the Earth’s oceanic crust and upper mantle. Ruthenium endemic isotope effects in chondrites and differentiated meteorites. Application of the Pt-Re-Os isotopic systems to mantle geochemistry and geochronology. Reviews in Mineralogy and Geochemistry, 81(1), 1–87.Ĭarlson, R. Experimental results on fractionation of the Highly Siderophile Elements (HSE) at variable pressures and temperatures during planetary and magmatic differentiation. Experimental constraints on the partitioning of Ru, Rh, Ir, Pt and Pd between chromite and silicate melt: the importance of ferric iron. Experimental constraints on the partitioning of rhenium and some platinum-group elements between olivine and silicate melt. Platinum-osmium isotope evolution of the Earth’s mantle: constraints from chondrites and Os-rich alloys. Geochimica et Cosmochimica Acta, 58(2), 705–716.īrandon, A. Solubility of palladium in silicate melts: implications for core formation in the Earth. The solubility of iridium in silicate melts: new data from experiments with Ir 10Pt 90 alloys. International Journal of Mass Spectrometry, 403, 15–26.īorisov, A., and Palme, H., 1995. Refinement of high precision Ru isotope analysis using negative thermal ionization mass spectrometry. ![]() Highly siderophile element composition of the Earth’s primitive upper mantle: constraints from new data on peridotite massifs and xenoliths. J., Gao, S., Lorand, J.-P., and Rudnick, R. ![]() ![]() The origin of the fractionation of platinum-group elements in terrestrial magmas. Dordrecht/Boston/London: Kluwer Academic Publishers, p. Siderophile element abundances in the upper mantle – evidence for a sulfide signature and equilibrium with the core. Non-chondritic distribution of the highly siderophile elements in mantle sulfides. ![]()
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