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Updated: Jul 12, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

トングステンのイソトープは,マントルの羽根が地球の核からの貢献を含まないという証拠です

Anders Scherstén1, Tim Elliott, Chris Hawkesworth

  • 1Department of Earth Sciences, University of Bristol, Will's Memorial Building, Queen's Road, Bristol BS8 1RJ, UK. anders.schersten@bristol.ac.uk

Nature
|January 16, 2004
PubMed
まとめ

海洋島ベサルトのボルンゲンイソトープは,コア・マントルの混合モデルをサポートしていません. これは,コア相互作用ではなく,リサイクルされた海洋地殻が,これらの玄武岩のオスミウム同位体異常を説明することを示唆しています.

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