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Updated: Apr 2, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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マントル硫化物における高度サイドロフィール元素の非コンドリート分布

O Alard1, W L Griffin, J P Lorand

  • 1GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, New South Wales, Australia. oalard@laurel.ocs.mq.edu.au

Nature
|November 1, 2000
PubMed
まとめ

地球のマントル岩の高度サイドロフィール元素 (HSE) のパターンはコンドリートではない. 代わりに,硫化物の変動は,核や隕石の追加ではなく,融解やメタソマチズムなどの上層マントルのプロセスを明らかにします.

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