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Updated: May 8, 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

地球のマントルの酸化状態を設定する 深いマグマの海洋形成

Katherine Armstrong1, Daniel J Frost2, Catherine A McCammon1

  • 1Bayerisches Geoinstitut, University of Bayreuth, D-95447 Bayreuth, Germany.

Science (New York, N.Y.)
|August 31, 2019
PubMed
まとめ

地球の初期の大気は,金属鉄が核に分離するにつれて,より酸化した. この過程は二酸化炭素が ダイヤモンドとして沈殿することを可能にすることで 惑星の炭素豊富な内部も説明します

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