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Updated: Jan 23, 2026

Determination of Aggregate Surface Morphology at the Interfacial Transition Zone ITZ
08:59

Determination of Aggregate Surface Morphology at the Interfacial Transition Zone ITZ

Published on: December 16, 2019

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マントルの移行領域の深さにおける寒い潜水板における磁気

I Kupenko1, G Aprilis2,3, D M Vasiukov2,3,4

  • 1Institut für Mineralogie, University of Münster, Münster, Germany. kupenko@uni-muenster.de.

Nature
|June 7, 2019
PubMed
まとめ

地球のマントルの鉄に富んだヘマタイト (α-Fe2O3) は,深層の移行領域の深さでも磁性であり,逆転時に潜在的に深層の磁気異常と仮想地磁気極の経路を説明します.

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