地球下层地幔的结构和动态
Edward J Garnero1, Allen K McNamara
1School of Earth and Space Exploration, Arizona State University, Box 871404, Tempe, AZ 85287, USA. garnero@asu.edu
概括
地球下层地幔的动态对于行星进化至关重要. 地震和矿物物理数据揭示了深层地幔结构,包括不同的省份和矿到矿后阶段过渡.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 行星科学 行星科学
背景情况:
- 地球下层地幔的过程显著影响着行星的进化.
- 了解这些过程需要整合地震和矿物物理数据.
- 深层地幔结构,就像大型低剪切速度的省份一样,表明化学上是不同的材料.
研究的目的:
- 将最近的地震和矿物物理发现合成地球下层地幔的地力学一致模型.
- 解释深层地幔结构及其对行星进化的影响.
主要方法:
- 高分辨率地震学研究的分析.
- 集成矿物物理数据的相位过渡.
- 地力学建模用于评估解释的可行性.
主要成果:
- 确定了两个大型的,相反的低切割速度的省份,可能由更密集的,化学上不同的材料组成.
- 观测地震速度的不连续性与最深层地幔中矿到矿后阶段过渡相一致.
- 通过超低地震速度的口袋,潜在地识别了深层岩腔.
结论:
- 地球的下层地幔表现出复杂的结构和化学异质.
- 矿过渡到后矿过渡是深层地幔的一个关键特征.
- 对深层地幔结构的进一步研究可能会揭示洞察诸如岩腔等过程.
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