Prediction of siderophile element metal-silicate partition coefficients to 20 GPa and 2800°C: the effects of pressure, temperature, oxygen fugacity, and silicate and metallic melt compositions
- 1 March 1997
- journal article
- conference paper
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 100 (1-4) , 115-134
- https://doi.org/10.1016/s0031-9201(96)03235-9
Abstract
No abstract availableThis publication has 61 references indexed in Scilit:
- Partitioning of Tungsten and Molybdenum Between Metallic Liquid and Silicate MeltScience, 1995
- Partitioning of elements among two silicate perovskites, superphase B, and volatile-bearing melt at 23 GPa and 1500–1600°CEarth and Planetary Science Letters, 1995
- Melting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPaJournal of Geophysical Research, 1994
- Effect of water on melting phase relations and melt composition in the system Mg2SiO4MgSiO3H2O up to 15 GPaPhysics of the Earth and Planetary Interiors, 1994
- High-Pressure and High-Temperature Experiments on Core-Mantle Segregation in the Accreting EarthScience, 1994
- Superheating Effects on Metal-Silicate Partitioning of Siderophile ElementsScience, 1993
- Activity of Nickel(II) Oxide in Silicate MeltsJournal of the American Ceramic Society, 1992
- On the chalcophile character of molybdenum: determination of sulfide/silicate partition coefficients of Mo and WEarth and Planetary Science Letters, 1991
- Transition metal partitioning between lower mantle and core materials at 27 GPaGeophysical Research Letters, 1991
- The primodial terrestrial magma ocean and its implication for stratification of the mantlePhysics of the Earth and Planetary Interiors, 1985