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• W2000534851 abstract "[1] Perovskite in the starting composition of Mg3Fe3+AlSi3O12 was investigated at 24 and 51 GPa and 2100 K using a laser-heated diamond anvil cell (LHDAC) and an analytical transmission electron microscopy (ATEM) to understand the solubilities of Fe3+ and Al into MgSiO3-dominated perovskite. A single phase of orthorhombic perovskite was formed at 51 GPa and 2100 K and the Fe3+AlO3 bearing perovskite showed no structural change during decompression. The samples synthesized at 24 GPa and 2100 K showed minor amounts of magnesioferrite and stishovite phases in spaces along the perovskite grain boundaries. These results indicate that the solubility of ferric iron incorporated as the Fe3+AlO3 component in MgSiO3-based perovskite is higher and slightly lower than 25 mole % at 51 and 24 GPa, respectively." @default.
• W2000534851 created "2016-06-24" @default.
• W2000534851 creator A5043339036 @default.
• W2000534851 date "2005-01-01" @default.
• W2000534851 modified "2023-10-17" @default.
• W2000534851 title "Fe³⁺and Al solubilities in MgSiO₃perovskite: implication of the Fe³⁺AlO₃substitution in MgSiO₃perovskite at the lower mantle condition" @default.
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• W2000534851 doi "https://doi.org/10.1029/2005gl023529" @default.
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