在地球上层地幔深处有水的地震证据
Mark van der Meijde1, Federica Marone, Domenico Giardini
1Institute of Geophysics, Eidgenössische Technische Hochschule-Hönggerberg (HPP)/Swiss Federal Institute of Technology CH-8093 Zürich, Switzerland. mark@tomo.ig.erdw.ethz.ch
概括
深层上层地幔水对地震不连续性产生重大影响. 一个410公里的不连续性,厚度为20-35公里,可能含有多达700ppm的水,影响地幔过渡区属性.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 矿物物理 矿物物理
背景情况:
- 地幔过渡区 (MTZ) 呈现地震不连续性.
- 水含量是影响地幔特性和地震波行为的一个关键因素.
研究的目的:
- 为了研究深层上地幔水对地震不连续性的影响.
- 为了确定导致特定MTZ不连续性的水含量.
主要方法:
- 对转换的地震波的分析.
- 通过异质地幔结构建模地震波传播.
主要成果:
- 在大约410公里深处,有20至35公里厚的地震断裂的证据.
- 这种不连续性最好解释为存在大量的水,估计高达每百万分之700的重量.
结论:
- 深层上层地幔水在塑造地震不连续性的特性方面发挥着至关重要的作用.
- 观察到的410公里不连续性很可能是水性相极限或受水性矿物质的影响.
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