在地球深层地幔中发生的氧化还原结和融化是碳铁氧化还原合导致的
1Institut für Geochemie und Petrologie, ETH Zürich, Sonneggstrasse 5, 8092 Zürich, Switzerland. arno.rohrbach@gmail.com
Nature
|March 29, 2011
概括
在地球深处碳酸盐引起的融化.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 地震学 地震学
背景情况:
- 沉降的海洋石化层可以将碳酸盐运送到深层地幔.
- 碳酸盐的存在与地震速度异常和地幔融化有关.
- 上层地幔的融化通常是由少量的碳酸盐引发的.
研究的目的:
- 为了研究碳酸盐诱导的融化在地球深层的过渡区和下层地幔.
- 为了了解碳酸盐在地幔回收过程中融化的命运.
- 为了解释深层地幔融化的形成.
主要方法:
- 实验性石油学模拟地球深层条件.
- 分析融的稳定性和转化.
- 在地幔矿物中研究氧化还原条件和铁的物种化.
主要成果:
- 碳酸盐融在环境地幔中不稳定,在~250公里深度以下转化为钻石.
- 一个"redox结"的过程使碳不动化成钻石,保存Fe3+).
- 在上井过程中,钻石与保存的Fe3+反应,导致在660公里和250公里处的氧化还原化.
结论:
- 碳酸盐诱导的融化可以发生在深度沉积的石化层中.
- 反氧结和随后的融化解释了深层融化的产生.
- 这一过程有助于地幔异质性和深层碳循环.
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