Melting and defect transitions in FeO up to pressures of Earth’s core-mantle boundary
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DOI: 10.1038/s41467-023-43154-w
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References listed on IDEAS
- T. Kimura & H. Ohfuji & M. Nishi & T. Irifune, 2017. "Melting temperatures of MgO under high pressure by micro-texture analysis," Nature Communications, Nature, vol. 8(1), pages 1-7, August.
- Sebastian Rost & Edward J. Garnero & Quentin Williams & Michael Manga, 2005. "Seismological constraints on a possible plume root at the core–mantle boundary," Nature, Nature, vol. 435(7042), pages 666-669, June.
- S. Labrosse & J. W. Hernlund & N. Coltice, 2007. "A crystallizing dense magma ocean at the base of the Earth’s mantle," Nature, Nature, vol. 450(7171), pages 866-869, December.
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Cited by:
- Wai-Ga D. Ho & Peng Zhang & Kristjan Haule & Jennifer M. Jackson & Vladimir Dobrosavljević & Vasilije V. Dobrosavljevic, 2024. "Quantum critical phase of FeO spans conditions of Earth’s lower mantle," Nature Communications, Nature, vol. 15(1), pages 1-8, December.
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