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Updated: May 23, 2025

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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可变的地幔氧化还原状态是由深度沉降的碳驱动的

Mingdi Gao1, Yu Wang1, Stephen F Foley2,3

  • 1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.

Science advances
|May 21, 2025
PubMed
概括

岩石沉积驱动了地幔氧化还原变化,影响了钻石的形成. 在深层地幔中,碳酸盐与金属铁 (Fe0) 的融化反应会在坑下形成明显的减少或氧化条件.

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