Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6438783 | Geochimica et Cosmochimica Acta | 2014 | 21 Pages |
Abstract
The solubility of Pt in silicate melt was investigated at conditions of 2073-2573Â K, 2Â GPa and â¼IW â1.5 to +3.5. These are the first measurements of Pt solubility under conditions more reducing than the iron-wüstite buffer (IW) which are demonstrably free from contamination by metal-inclusions. Pt solubility increases with increasing temperature and decreasing oxygen fugacity. The ability of carbon to enhance Pt solubility under reducing conditions (3500Â K. Under these conditions however, the estimated Pt/Os ratio is â¼40,000 times higher than that estimated for the PUM (Brandon et al., 2006). Instead, the PUM composition is generated most readily by metal-silicate equilibrium at more modest temperatures (â¼3100Â K), followed by a late accretion of chondritic material subsequent to core formation.
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Authors
N.R. Bennett, J.M. Brenan, K.T. Koga,