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Updated: May 15, 2026

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

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Published on: November 15, 2013

ニッケルとヘリウムの証拠は,核-マントルの境界線上での融解の証拠です

Claude Herzberg1, Paul D Asimow, Dmitri A Ionov

  • 1Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, New Jersey 08854-8066, USA. herzberg@rci.rutgers.edu

Nature
|January 11, 2013
PubMed
まとめ

玄武岩のヘリウム3とヘリウム4の比率が高いことは,地上の深い源からの起源を示唆しています. このニッケルが豊富で,ガスが少ないマントルの源は,地球の歴史の初期に,コアとマントルの相互作用によって形成された可能性が高い.

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