Melting curve of (Mg,Fe)SiO3 perovskite to 96 GPa: Evidence for a structural transition in lower mantle melts
- 1 May 1989
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 16 (5) , 421-424
- https://doi.org/10.1029/gl016i005p00421
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Density and composition of the lower mantlePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1989
- Spectroscopic Evidence for Pressure-Induced Coordination Changes in Silicate Glasses and MeltsScience, 1988
- Densities of Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-TiO2-SiO2 liquids: New measurements and derived partial molar propertiesGeochimica et Cosmochimica Acta, 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
- Thermal expansion of silicate perovskite and stratification of the Earth's mantleNature, 1986
- Densities of Liquid Silicates at High PressuresScience, 1984
- Stability Relations of Silicate Spinels, Ilmenites, and PerovskitesPublished by Springer Nature ,1982
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- MELTING AT HIGH PRESSURESSoviet Physics Uspekhi, 1969