水性地幔过渡区以环木石表示,包含在钻石中
D G Pearson1, F E Brenker2, F Nestola3
1Department of Earth and Atmospheric Sciences, 1-26 Earth Sciences Building, University of Alberta, Edmonton, Alberta T6G 2E3, Canada.
Nature
|March 14, 2014
概括
地球深层地幔过渡区可能有大量的水. 研究人员在巴西钻石中发现了富含水的环木石的证据,证实该区域在当地是水性.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 地震学 地震学
背景情况:
- 地球的过渡区 (深度为410-660公里) 被认为是一个主要的水库.
- 高压橄烯多态 (wadsleyite,ringwoodite) 可以储存大量的水.
- 关于过渡区水分的地质数据仍然存在争议.
研究的目的:
- 提供直接证据,证明高压橄烯多态的陆地发生.
- 为了研究地球过渡区的水含量.
主要方法:
- 在X射线中,X射线的衍射效果是不同的.
- 拉曼光谱法 拉曼光谱法
- 红外光谱学 红外光谱学 红外光谱学
- 来自巴西Juína的钻石包装的分析.
主要成果:
- 第一个陆地证据表明木,一个高压的橄烯多态.
- 环木含有丰富的水 (大约. 在重量上占1%.
- 环木的保存表明一个水性过渡区.
结论:
- 地球的过渡区被证实是局部含水的.
- 这一发现支持了水性过渡区在岩石和板块构造学中的作用.
- 一些金伯石可能起源于这个深层地幔区域.
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