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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

地球のコア・マントル境界:高圧・高温での実験結果

E Knittle, R Jeanloz

    Science (New York, N.Y.)
    |March 22, 1991
    PubMed
    まとめ

    液体鉄は,マントルシリケートと極端な圧力で反応し,新しい合金や鉱物を形成します. 地球のD"層におけるこれらの反応は,地震波の異常を説明し,地力学に影響を与える可能性があります.

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