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Updated: Jul 12, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
地幔中的大陆-海洋化学异质性基于地震断层扫描
概括
地幔地震模型揭示了大陆与海洋之间的显著差异,不仅仅是温度. 地质逆转表明,上层地幔的组成变化解释了这些地震异质性,而不仅仅是热效应.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地力学是什么?地力学是什么?
背景情况:
- 全球地震模型揭示了大陆和海洋下方明显的侧面地幔异质性.
- 这些地震差异超过了仅归因于热变化的差异.
研究的目的:
- 研究大陆和海洋上层地幔之间的系统地震差异的起源.
- 确定构成变化是否有助于观察到的地幔异质性.
主要方法:
- 利用全球规模侧面地幔异质性的地震模型.
- 进行了地质逆转,结合了粘性地幔流.
- 将地震数据与地形数据集成,以推断密度和组成.
主要成果:
- 大陆和海洋下面的地震差异太大了,不能单靠热源来解释.
- 地形逆转表明上层地幔的组成差异,以及热异质性,解释了地震变化.
- 大陆和海洋上层地幔之间的净密度差异很小.
结论:
- 上层地幔的组成变化在解释大陆和海洋下方的地震异质性方面发挥着至关重要的作用.
- 热和组成异质性的相互作用支配了地幔结构.
- 低质量和热流穿过天气层和地幔过渡区与观察到的密度差异一致.
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