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Updated: Dec 9, 2025

Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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超深層のダイヤモンドに記録された石層から下層のマントルへの炭素循環

M E Regier1, D G Pearson2, T Stachel2

  • 1Canadian Centre for Isotopic Microanalysis, Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada. margoregier@gmail.com.

Nature
|September 10, 2020
PubMed
まとめ

沈殿物ではなく 炭酸化海殻が 深い地層の炭素の 主な源です ダイヤモンドインクルージョンは,この炭素を移行領域に吸収し,ダイヤモンドと下層マントルの炭素バリアを形成します.

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