Crystallization of silicon dioxide and compositional evolution of the Earth’s core
Kei Hirose (),
Guillaume Morard,
Ryosuke Sinmyo,
Koichio Umemoto,
John Hernlund,
George Helffrich and
Stéphane Labrosse
Additional contact information
Kei Hirose: Earth-Life Science Institute, Tokyo Institute of Technology
Guillaume Morard: Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, UMR CNRS 7590, Sorbonne Universités—Université Pierre et Marie Curie, CNRS, Muséum National d’Histoire Naturelle, IRD
Ryosuke Sinmyo: Earth-Life Science Institute, Tokyo Institute of Technology
Koichio Umemoto: Earth-Life Science Institute, Tokyo Institute of Technology
John Hernlund: Earth-Life Science Institute, Tokyo Institute of Technology
George Helffrich: Earth-Life Science Institute, Tokyo Institute of Technology
Stéphane Labrosse: Université de Lyon, École normale supérieure de Lyon, Université Lyon-1, CNRS, UMR 5276 LGL-TPE
Nature, 2017, vol. 543, issue 7643, 99-102
Abstract:
Melting experiments with liquid Fe–Si–O alloy at the pressure of the Earth’s core reveal that the crystallization of silicon dioxide leads to core convection and a dynamo.
Date: 2017
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:543:y:2017:i:7643:d:10.1038_nature21367
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DOI: 10.1038/nature21367
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