在地幔过渡区的全球玄武岩积累的地震证据
Chunquan Yu1,2, Saskia Goes3, Elizabeth A Day3
1Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, China.
Science advances
|May 31, 2023
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 地球地幔的组成对于理解其热化学演变至关重要,但仍有争议.
- 之前的研究缺乏足够的数据来准确地解决地幔组成.
研究的目的:
- 为了确定地球地幔的辐射平均组成.
- 为了研究地幔过渡区的组成结构.
主要方法:
- 对反映在410公里和660公里不连续性的地震波 (剪切和压缩) 的大型全球数据集的分析.
- 阵列分析以检索SS和PP前体反射率的振幅距离趋势.
- 推断相对波速和密度对比以确定地幔组成.
主要成果:
- 地幔过渡区富含玄武岩,在660公里不连续性 (~40%) 附近的玄武岩分量高于410公里不连续性 (~18-31%).
- 地震数据显示,地幔中含有玄武岩的过渡区,这与地幔对流和板块回收模型相一致.
- 结果表明,整体地幔的二氧化含量比火石基准成分更高.
结论:
- 岩地积在地幔过渡区,在660公里不连续性附近达到峰值.
- 地幔的组成比简化的火石模型更复杂.
- 地震数据为地幔组成和演变提供了强烈的约束.
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