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Updated: May 16, 2026

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

マントルに溶けた鉄の深い浸透は,形態学的不安定性によって引き起こされる

Kazuhiko Otsuka1, Shun-ichiro Karato

  • 1Department of Geology and Geophysics, Yale University, 210 Whitney Avenue, New Haven, Connecticut 06511, USA.

Nature
|December 14, 2012
PubMed
まとめ

新しいメカニズムは,地球のマントルの奥深くにある鉄の濃縮を説明する. 形態学的不安定性により,鉄に富んだ液体がマントルに浸透し,鉄をコア-マントル境界から遠くに運ぶことができます.

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