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Updated: May 11, 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

地球の内核の境界にある鉄の融解は,急速なX線 difrakcionによるものです

S Anzellini1, A Dewaele, M Mezouar

  • 1Commissariat à l'Énergie Atomique, Direction des Applications Militaires, Île de France, Arpajon Cedex, France. simone.anzellini@cea.fr

Science (New York, N.Y.)
|April 27, 2013
PubMed
まとめ

研究者らは,地球の内核の境界にある鉄の融点を決定した. この発見は,コア-マントルの境界で高い熱流が起こり,マントルの部分的な融解を引き起こす可能性があることを示唆しています.

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