Partitioning magnesium perovskite/melt

The lower mantle is made predominantly of magnesium perovskite, and thus a solid understanding of element partitioning between perovskite and silicate melt is relevant to the early history of the Earth. Much of the early work with perovskite was done on aluminum-free or low-aluminum materials. However, magnesium perovskite can accommodate AI2O3 into its structure (Wood, 2000 Stebbins et ai, 2001),... 

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