在美国西部以下探测了天气密度,温度和弹性模块
1Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. takeo_ito@nagoya-u.jp
概括
海洋的潮揭示了地球的地球.
科学领域:
- 地质物理学 地质物理学
- 固体地球科学 固体地球科学
- 地震学 地震学
背景情况:
- 海洋潮对地球表面施加周期性负荷.
- 这些潮负荷导致可测量的表面移位.
- 了解这些反应为我们提供了对地球内部的洞察.
研究的目的:
- 为了建模地球地和上层地幔结构.
- 为了独立估计密度和弹性模块.
- 为了研究美国西部下面的天气层.
主要方法:
- 使用地质观测对表面移位的观测.
- 分析海洋潮负载引起的移位.
- 开发一个深度依赖的地球物理模型.
主要成果:
- 在天气层边界确定了密度和弹性剪切模块的强度梯度.
- 在220公里深处没有发现离散的结构不连续性.
- 在天气层中限制了低密度异常 (~50 kg/m3).
结论:
- 一个~300°C的温度异常解释了天气层的低密度和弹性模块.
- 海洋潮负荷是探索地球结构的可行方法.
- 美国西部下面的天气层表现出显著的变化.
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