Melting boundary of Fe‐17%Si up to 5.5 GPa and the timing of core formation
- 15 January 1999
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 26 (2) , 263-266
- https://doi.org/10.1029/1998gl900292
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Core formation and chemical equilibrium in the Earth—I. Physical considerationsPhysics of the Earth and Planetary Interiors, 1997
- High-Pressure Iron-Sulfur Compound, Fe 3 S 2 , and Melting Relations in the Fe-FeS SystemScience, 1997
- Constraints on core chemistry from the pressure dependence of the bulk modulusPhysics of the Earth and Planetary Interiors, 1997
- Thermal and chemical evolution of the terrestrial magma oceanPhysics of the Earth and Planetary Interiors, 1997
- Hafnium–tungsten chronometry and the timing of terrestrial core formationNature, 1995
- High p, T physical property studies of Earth's interior: Thermoelectric power of solid and liquid Fe up to 6.4 GPaCanadian Journal of Physics, 1995
- Mechanisms of Earth differentiation: Consequences for the chemical structure of the mantleReviews of Geophysics, 1994
- Light elements in the Earth's outer core: A critical reviewPhysics of the Earth and Planetary Interiors, 1994
- Physical state of the very early EarthLithos, 1993
- Earth and Mars: early thermal profilesPhysics of the Earth and Planetary Interiors, 1983