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
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