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Updated: May 27, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Published on: November 15, 2013

FeOの相変化と,地球の外核の層格化

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
まとめ

鉄一酸化物 (FeO) は,極端な圧力下では新しい段階に変化し,地球の核の性質を変更します. この変化はコンベクションを抑制し,ジオダイナモに影響を及ぼします.

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