Maximum solubility of FeO in (Mg, Fe)SiO3‐perovskite as a function of temperature at 26 GPa: Implication for FeO content in the lower mantle
- 10 May 1996
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 101 (B5) , 11525-11530
- https://doi.org/10.1029/96jb00408
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Material transport in laser‐heated diamond anvil cell melting experimentsGeophysical Research Letters, 1992
- SILICATE PEROVSKITEAnnual Review of Earth and Planetary Sciences, 1992
- Experimental determination of element partitioning and calculation of phase relations in the MgO‐FeO‐SiO2 system at high pressure and high temperatureJournal of Geophysical Research, 1991
- Constraints on lower mantle composition and temperature from density and bulk sound velocity profilesGeophysical Research Letters, 1990
- Postspinel transformations in the system Mg2SiO4‐Fe2SiO4 and some geophysical implicationsJournal of Geophysical Research, 1989
- Transformation of enstatite ? diopside ? jadeite pyroxenes to garnetContributions to Mineralogy and Petrology, 1989
- Density and composition of the lower mantlePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1989
- Acquisition of Powder Diffraction Data with Synchrotron RadiationAustralian Journal of Physics, 1988
- The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgO FeO SiO2Earth and Planetary Science Letters, 1984
- Stability Relations of Silicate Spinels, Ilmenites, and PerovskitesPublished by Springer Nature ,1982