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Updated: May 8, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 16, 2013

マントルのメタソマチズムの証拠は,海底の海殻からの水性シリシウム溶液によるものです

G Prouteau1, B Scaillet, M Pichavant

  • 1UMR 6538, UBO, 6 avenue Le Gargeu, P.B. 809, 29285 Brest, France.

Nature
|March 10, 2001
PubMed
まとめ

流体だけでなく,スラブ由来の溶融は,潜水地帯のマントル岩を変化させることができます. これらのシリカ濃度の高い融解は,島弧の玄武岩における低ニオビウム,タンタール,およびタイタンの存在を説明し,融解メタソマチズムは以前に考えられていたよりも一般的であることを示唆しています.

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