水和潜伏区岩石的氧化状态
Katherine A Kelley1, Elizabeth Cottrell
1Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA. kelley@gso.uri.edu
概括
地幔氧气流动性,对地球至关重要.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 地幔氧气流动性控制着地球的内部和外部质量交换.
- 影响地幔氧气流动性及其演变的因素受到争议.
研究的目的:
- 调查对地幔氧气流失的控制.
- 将构造周期与地幔氧化状态联系起来.
主要方法:
- 使用Fe K边缘微型X射线吸收近边缘结构光谱测量Fe3+/SigmaFe比率.
- 在玄武岩玻璃和融化内含物中分析爆发前的岩H2O含量.
- 在多样化的板块构造设置中进行全球采样.
主要成果:
- 岩石Fe3+/SigmaFe比率在俯冲区的方向上增加 (斜坡:0.13-0.17,背弧:0.15-0.19,弧:0.18-0.32).
- Fe3+/SigmaFe比率与岩中的H2O含量线性相关.
- 观察到的相关性与板块衍生流体的元素标记物联系在一起.
结论:
- 从潜浮板块的质量转移直接氧化了地幔.
- 挥发性和板块衍生的流体是地幔氧化的主要驱动因素.
- 提供了关于地幔的氧化还原演变的见解.
相关概念视频
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