Solubilities of O and Si in liquid iron in equilibrium with (Mg,Fe)SiO3 perovskite and the light elements in the core
- 30 March 2005
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 32 (6)
- https://doi.org/10.1029/2005gl022773
Abstract
No abstract availableThis publication has 18 references indexed in Scilit:
- Another look at the core density deficit of Earth’s outer corePhysics of the Earth and Planetary Interiors, 2002
- Chemical composition of the Earth and the volatility control on planetary geneticsEarth and Planetary Science Letters, 2001
- Physics of Iron at Earth's Core ConditionsScience, 2000
- High Pressure Reactions Between Metals and Silicates: Implications for the Light Element in the Core and Core-Mantle InteractionsMineralogical Magazine, 1998
- Thermodynamic data for phases in the FeO-MgO-SiO2 system and phase relations in the mantle transition zonePhysics and Chemistry of Minerals, 1995
- Reactions between molten iron and silicate melts at high pressure: Implications for the chemical evolution of Earth's coreJournal of Geophysical Research, 1995
- High‐pressure and high‐temperature reactions between silicates and liquid iron alloys, in the diamond anvil cell, studied by analytical electron microscopyJournal of Geophysical Research, 1992
- Earth's Core-Mantle Boundary: Results of Experiments at High Pressures and TemperaturesScience, 1991
- Composition of the core and implications for origin of the earth.GEOCHEMICAL JOURNAL, 1977
- Density and composition of mantle and coreJournal of Geophysical Research, 1964