全波形断层扫描揭示了铁自旋交叉在地球的下层地幔
Laura Cobden1, Jingyi Zhuang2, Wenjie Lei2,3,4
1Department of Earth Sciences, Utrecht University, 3584 CB Utrecht, Utrecht, The Netherlands. l.j.cobden@uu.nl.
Nature communications
|March 4, 2024
概括
三维地震模型揭示了地球下层地幔的温度变化. 这些模型确定了核心-地幔边界附近的矿物质旋转转变和缩,这表明了一个古老的岩海洋.
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:
- 一维地震模型掩盖了温度依赖的现象.
- 全波形断层扫描提供更高分辨率的3D地震波速映射.
- 绝对波速区分温度与组成或自旋状态变化.
研究的目的:
- 量化解释地球下层地幔中的地震波速.
- 用3D断层扫描来调查温度,组成和旋转状态变化.
- 测试地幔模型与地震波速度数据对比.
主要方法:
- 使用最近发表的全波形断层扫描模型.
- 批量和剪切波速度的联合解释.
- 将地震波速分布与假设的地幔组成进行比较.
主要成果:
- 下层地幔的波速多样性不能用同化学地幔来解释.
- 带有ferropericlase电子旋转交叉器的地幔模型更适合1000-2500公里深度之间的波速.
- 丰富解释了波速在2500公里以下的波速,可能来自岩海洋.
结论:
- 地震波的速度表明下层地幔的温度和组成变化很大.
- 在ferropericlase中的电子旋转交叉可能在中下层地幔中活跃.
- 在核心-地幔边界的缩表明早期岩海洋的残余.
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