在受羽毛影响的中海基岩中观察到的循环脱水石质层
Jacqueline Eaby Dixon1, Loretta Leist, Charles Langmuir
1RSMAS/MGG, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149, USA. jdixon@rsmas.miami.edu
Nature
|December 3, 2002
概括
将水回收到地球深层是不确定的. 这项研究表明,俯冲能有效地从海洋石化层中提取水,在这个过程中,超过92%的水被除去.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 地球科学 地球科学 地球科学
背景情况:
- 全球地质化学水循环的理解很少,特别是水的深层地幔循环.
- 海洋石化层的降温是一个关键的,但不确定的途径,用于将水输送到地球深处.
研究的目的:
- 为了研究水回收到深层地幔的效率.
- 使用玄武岩来描述不同地幔组成部分的挥发性物质含量.
主要方法:
- 在海洋岛基岩 (OIBs) 和中海基岩 (MORBs) 中挥发性含量的分析.
- 与不同地幔来源相关的OIB中含水量的比较,包括带有潜水石层 (EM类型) 的OIB.
主要成果:
- 海洋岛屿玄武岩通常含有比中海基岩更多的水.
- 与富含地幔 (EM类型) 组成部分相关的岩石,其中含有起的石化层,与普通地幔来源相比,其含水量减少.
- 这表明在潜水过程中有效提取水.
结论:
- 潜伏过程在从潜伏的海洋石化层中提取水的效率高 (>92%).
- 这项研究提供了对地球地幔内水运输和回收的机制的关键见解.
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