関連する実験動画

Updated: May 1, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

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大規模なマントルの融解と大陸の成長の間のリンクは,オスミウムイソトープで見られる

D G Pearson1, S W Parman, G M Nowell

  • 1Northern Centre for Isotopic and Elemental Tracing, Department of Earth Sciences, Durham University, South Road, Durham DH1 4QE, UK. d.g.pearson@durham.ac.uk

Nature
|September 14, 2007
PubMed
まとめ

地球の大陸の地殻は,連続的にではなく,パルスで成長した. オスミウムイソトープを用いた新しい研究は,マントルの枯渇イベントが地殻形成のピークと一致することを明らかにし,私たちの惑星の地殻のパルス成長モデルをサポートしています.

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