The effect of pressure on partitioning of Ni and Co between silicate and iron-rich metal liquids: a diamond-anvil cell study
- 15 April 2003
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 209 (1-2) , 245-255
- https://doi.org/10.1016/s0012-821x(03)00076-1
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Mechanisms of metal–silicate equilibration in the terrestrial magma oceanPublished by Elsevier ,2002
- The self-diffusion of silicon and oxygen in diopside (CaMgSi2O6) liquid up to 15 GPaChemical Geology, 2001
- Evidence for a late chondritic veneer in the Earth's mantle from high-pressure partitioning of palladium and platinumNature, 2000
- Metal-silicate equilibrium in a homogeneously accreting earth: new results for RePublished by Elsevier ,1998
- Oxide‐metal equilibria to 2500°C and 25 GPa: Implications for core formation and the light component in the Earth's coreJournal of Geophysical Research, 1998
- Element partitioning between metallic liquid, magnesiowustite, and silicate liquid at 20 GPa and 2500°C: A secondary ion mass spectrometric studyGeophysical Research Letters, 1996
- High-Pressure and High-Temperature Experiments on Core-Mantle Segregation in the Accreting EarthScience, 1994
- Core Formation During Early Accretion of the EarthScience, 1991
- Partitioning “equilibrium”, temperature gradients, and constraints on Earth differentiationEarth and Planetary Science Letters, 1989
- Constitution of terrestrial planetsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1981