Simulating the core‐mantle boundary: An experimental study of high‐pressure reactions between silicates and liquid iron
- 1 July 1989
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 16 (7), 609-612
- https://doi.org/10.1029/gl016i007p00609
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Lateral variations near the core‐mantle boundaryGeophysical Research Letters, 1988
- Electrical conductivity of (Mg,Fe)SiO3 perovskite and a perovskite‐dominated assemblage at lower mantle conditionsGeophysical Research Letters, 1987
- The Core-Mantle BoundaryAnnual Review of Earth and Planetary Sciences, 1987
- The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's CenterScience, 1987
- Synthesis and Equation of State of (Mg,Fe) SiO 3 Perovskite to Over 100 GigapascalsScience, 1987
- Scales of heterogeneity near the core‐mantle‐boundaryGeophysical Research Letters, 1986
- High‐pressure metallization of FeO and implications for the Earth's coreGeophysical Research Letters, 1986
- Metallization of Fe0.94O at elevated pressures and temperatures observed by shock-wave electrical resistivity measurementsSolid State Communications, 1986
- A crystal chemical study of stishoviteJournal of Solid State Chemistry, 1983
- Orthorhombic perovskite phases observed in olivine, pyroxene and garnet at high pressures and temperaturesPhysics of the Earth and Planetary Interiors, 1976