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Updated: May 23, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

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

Published on: June 13, 2015

最も初期のプラネティシマルの後の蓄積は,高度に siderophile 要素によって明らかにされています

Christopher W Dale1, Kevin W Burton, Richard C Greenwood

  • 1Department of Earth Sciences, Durham University, Durham DH1 3LE, UK. christopher.dale@durham.ac.uk

Science (New York, N.Y.)
|April 12, 2012
PubMed
まとめ

コンドリート物質の後期的蓄積は,惑星のマントルに含まれる高度な siderophile 元素 (HSEs) の豊富さを説明する. この過程は,すべての微分体に共通しており,酸化状態がHSE分布を制御している.

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