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Updated: May 2, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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アケア紀の地殻の進化は,デラミネーションと浅い潜水によるものでした

Stephen F Foley1, Stephan Buhre, Dorrit E Jacob

  • 1Institut für Geologische Wissenschaften, Universität Greifswald, Germany. sfoley@uni-greifswald.de

Nature
|January 17, 2003
PubMed
まとめ

初期の地球 初期の地球

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