Thermodynamics of the system Fe--FeO--MgO at high pressure and temperature and a model for formation of the Earth's core
Open Access
- 1 March 1983
- journal article
- Published by Oxford University Press (OUP) in Geophysical Journal International
- Vol. 72 (3), 577-595
- https://doi.org/10.1111/j.1365-246x.1983.tb02821.x
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- The pressure and temperature dependence of the elastic properties of polycrystal magnesiowustiteJournal of Geophysical Research: Solid Earth, 1982
- Melting of iron under core conditionsGeophysical Research Letters, 1980
- The current status of speculations on the composition of the core of the EarthReviews of Geophysics, 1976
- Melting of IronGeophysical Journal International, 1974
- Elasticity, crystal structure and phase transitionsEarth and Planetary Science Letters, 1974
- On planetary coresEarth, Moon, and Planets, 1973
- The viscosity of magmatic silicate liquids; a model calculationAmerican Journal of Science, 1972
- Die Phasenbildung von β‐W‐Strukturtyp in dünnen Schichten von Chrom, Molybdan und WolframCrystal Research and Technology, 1972
- Is the mantle soluble in the core?Journal of Geophysical Research, 1966
- Elasticity and constitution of the Earth's interiorJournal of Geophysical Research, 1952