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Updated: Feb 22, 2026

Atom Probe Tomography Analysis of Exsolved Mineral Phases
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35億年前のフェルシック地殻とプレート構造のチタン同位体証拠

Nicolas D Greber1, Nicolas Dauphas2, Andrey Bekker3,4

  • 1Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60615, USA. nicolas.greber@unige.ch.

Science (New York, N.Y.)
|September 23, 2017
PubMed
まとめ

プレート構造は地球の歴史の初期から 35億年前に始まり シェイルの構成が均一であったことが 証明されています この初期の活動は 栄養素供給と酸素レベルに影響を与えました

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