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Updated: May 4, 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

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一个脱气的岩上升到表面的氧化还原演变

Alain Burgisser1, Bruno Scaillet

  • 1ISTO, UMR 6113 Université d'Orléans-CNRS, 1a rue de la Férollerie, 45071 Orléans cedex 2, France. burgisse@cnrs-orleans.fr

Nature
|January 12, 2007
PubMed
概括

岩上升显著改变了火山气体的氧化还原状态,挑战了关于其与源头的联系的假设. 气体的组成和数量极大地影响了喷发期间的氧气流动性 (O2) 变化.

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