深水层地幔储备提供了33亿年前地回收的证据
Alexander V Sobolev1,2, Evgeny V Asafov3, Andrey A Gurenko4
1Université Grenoble Alpes, Université Savoie Mont Blanc, Institute Science de la Terre (ISTerre), CNRS, IRD, IFSTTAR, Grenoble, France. alexander.sobolev@univ-grenoble-alpes.fr.
Nature
|July 17, 2019
概括
在地球深处的水
科学领域:
- 地质化学和地质物理
- 地幔动力学
- 地球的早期演化
背景情况:
- 水显著影响地幔的特性,影响融化和对流.
- 追踪水的过程揭示了表面物质回收到深层地幔的过程,
- 科马提石来自地幔高度融化,是深层地幔组成和含水量的关键指标.
研究的目的:
- 在早期地球地幔中研究水的存在和起源.
- 为了确定深层,水化地幔水库存在于古考古时代.
- 在深层地幔中追踪海水改变的石化层的循环.
主要方法:
- 在古老的石中分析与 (D/H) 的比例.
- 包括水,和含量在内的科马提石融含量的地化学分析.
- 与表面储存,典型地幔和改变的海洋地的同位素组成进行比较.
主要成果:
- 古老的岩石 (年龄为33亿年) 显示出同位素的痕迹,表明它们的地幔来源是水.
- 这些发现证实了至少在古考古时期就存在深层水性地幔.
- 它的同位素成分表明海水改变了石化层,在沉积过程中脱水,被回收到深层地幔中.
结论:
- 自至少36亿年前以来,地球内部一直存在着深层水性地幔储存库.
- 海水的变化和石化层的沉降发生在33亿年前.
- 这种早期的回收影响了深层地幔的组成及其含水量.
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