Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4678406 | Earth and Planetary Science Letters | 2010 | 7 Pages |
Abstract
Soret separation of melts consisting of Fe (+ 1-10 wt.% Ni) with added C, Si or S and trace highly siderophile elements (HSE; Ru, Rh, Pd, Re, Os, Ir, Pt and Au) was investigated in experiments done at 2 GPa, Thot ~ 2000 °C and ThotâTcold ~ 250 °C. Experiments with added C and Si produced homogeneous samples, whereas those with S resulted in significant compositional gradients, with S enriched at the hot end of the sample, and Fe and HSE enriched at the cold end. The magnitude of the separation of the HSE is not the same for each, but varies in the order (smallest to largest) Pd~Au
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
James M. Brenan, Neil Bennett,