関連する実験動画

Updated: Jul 12, 2026

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

アシンメトリックな加熱を伴う大陸の漂流

L Knopoff, K A Poehls, R C Smith

    Science (New York, N.Y.)
    |June 2, 1972
    PubMed
    まとめ

    実験室のモデルは,粘性のあるアステノスフィアを通って石層のラフトを推進することによって,大陸の漂移をシミュレートします. 海洋と大陸の地殻における異なる熱濃度が,このシミュレートされたプレート移動を駆動している.

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