核心旋转动力学和地质事件
1Department of Geomagnetism and Paleomagnetism, Institut de Physique du Globe de Paris, 4 place Jussieu, 75252 Paris 05, France. Ecole et Observatoire des Sciences de la Terre, 5 rue R. Descartes, 67084 Strasbourg, France.
地球的流体核心和太阳的潮波在过去产生了共振,这可能解释了大陆地的形成和地球磁场逆转的变化.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 行星科学 行星科学
背景情况:
- 地球的流体核心动力学受到月球-太阳的潮力量的影响.
- 由于潮力,地球的轴旋转经历了长期减速.
研究的目的:
- 为了研究地球流体核心旋转自频和太阳潮波之间的共振的含义.
- 探索潮力,核心动力学和地质/地物理现象之间的联系.
主要方法:
- 分析由潮力引起的流体核心振荡.
- 检查地球轴旋转的潮世俗减速.
- 在核心边界的粘磁摩擦力的建模.
主要成果:
- 大约在3.0×10^9,1.8×10^9和3×10^8年前发生了共振事件.
- 核心边界的强磁摩擦会产生热量,破坏D"热层的稳定.
- 核心动力发电机过程的干扰是由流体核心边界温度升高引起的.
结论:
- 响应诱导的加热可能会触发深层地幔羽毛的产生.
- 这些现象可以解释大规模的大陆地形成和洪水玄武岩事件.
- 地磁逆转频率的突然变化可能与这些核心过程有关.
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