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Updated: May 27, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

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Published on: November 15, 2013

Transición de fase de FeO y estratificación en el núcleo externo de la Tierra

Haruka Ozawa1, Futoshi Takahashi, Kei Hirose

  • 1Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan. h-ozawa@jamstec.go.jp

Science (New York, N.Y.)
|November 15, 2011
PubMed
Resumen

El monóxido de hierro (FeO) se transforma en una nueva fase a presiones extremas, alterando las propiedades del núcleo de la Tierra. Este cambio suprime la convección, lo que afecta a la geodinámica.

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