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スピン・クロスオーバーと鉄に富んだシリケートが,地球の深いマントルで溶ける

Ryuichi Nomura1, Haruka Ozawa, Shigehiko Tateno

  • 1Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.

Nature
|April 26, 2011
PubMed
まとめ

地球の深いマントルの極端な圧力下では,鉄に富んだシリケート溶液は固体より密度が高くなります. 鉄のスピン・クロスオーバーによって引き起こされるこの密度逆転は,惑星の進化とコア-マントルの境界構造に深い意味を持ちます.

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