Composition of the core, II. Effect of high pressure on solubility of FeO in molten iron
- 30 November 1984
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 71 (1), 94-103
- https://doi.org/10.1016/0012-821x(84)90055-4
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Composition of the core, I. Solubility of oxygen in molten iron at high temperaturesEarth and Planetary Science Letters, 1984
- The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgO FeO SiO2Earth and Planetary Science Letters, 1984
- Some geophysical constraints on the chemical composition of the earth's lower mantleEarth and Planetary Science Letters, 1983
- The Earth's core and the phase diagram of ironPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1982
- High-pressure polymorphism of the iron oxidesGeophysical Journal of the Royal Astronomical Society, 1981
- Experimental approach to the state of the core; Part I, The liquidus relations of the Fe-rich portion of the Fe-Ni-S system from 30 to 100 kbAmerican Journal of Science, 1975
- Composition and Evolution of the Mantle and CoreScience, 1971
- On the Existence of Ternary Transition Metal Oxides.Acta Chemica Scandinavica, 1954
- On the Existence of Metallic Ternary Oxides Me'Me''O with the Metal Atoms in Hexagonal Close-packing.Acta Chemica Scandinavica, 1954
- The System Iron—Oxygen. II. Equilibrium and Thermodynamics of Liquid Oxide and Other PhasesJournal of the American Chemical Society, 1946