Reactions between molten iron and silicate melts at high pressure: Implications for the chemical evolution of Earth's core
- 10 April 1995
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 100 (B4) , 5901-5910
- https://doi.org/10.1029/94jb02645
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Melting of Ferromagnesian Silicates Under the Lower Mantle ConditionsPublished by Wiley ,2013
- Dissolution of K in molten iron at high pressure and temperatureGeophysical Research Letters, 1993
- 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
- Dissolution of Silicon and Oxygen in Molten Iron at High Pressure and Temperature.Proceedings of the Japan Academy, Series B, 1991
- Melting, thermal expansion, and phase transitions of iron at high pressuresJournal of Geophysical Research, 1990
- Postspinel transformations in the system Mg2SiO4‐Fe2SiO4 and some geophysical implicationsJournal of Geophysical Research, 1989
- Simulating the core‐mantle boundary: An experimental study of high‐pressure reactions between silicates and liquid ironGeophysical Research Letters, 1989
- The Earth's core formation due to the Rayleigh-Taylor instabilityIcarus, 1987
- Densities of liquid silicate systems calculated from partial molar volumes of oxide componentsAmerican Journal of Science, 1970