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Chemical interaction of Fe and Al2O3 as a source of heterogeneity at the Earth's core-mantle boundary

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Fabrichnaya,  O.
Former Dept. Materials Synthesis and Microstructure Design, Max Planck Institute for Intelligent Systems, Max Planck Society;

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Dubrovinsky, L., Annerstin, H., Dubrovinskaia, N., Westman, F., Harryson, H., Fabrichnaya, O., & Carlson, S. (2001). Chemical interaction of Fe and Al2O3 as a source of heterogeneity at the Earth's core-mantle boundary. Nature, 412(6846), 527-529.


引用: https://hdl.handle.net/11858/00-001M-0000-0010-3460-E
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