Chemical equilibrium between ferropericlase and molten iron to 134 GPa and implications for iron content at the bottom of the mantle

Title
Chemical equilibrium between ferropericlase and molten iron to 134 GPa and implications for iron content at the bottom of the mantle
Authors
Keywords
-
Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 35, Issue 5, Pages -
Publisher
American Geophysical Union (AGU)
Online
2008-03-11
DOI
10.1029/2007gl032648

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