地磁轴性二极极对热核-地幔相互作用的灵敏度
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA. jeremy_bloxham@harvard.edu
Nature
|May 16, 2000
概括
地球的磁场可能并不总是遵循地球中心轴心双极 (GAD) 模型. 数字模拟表明核心-地幔边界的热流变化,而不是内核大小,可能解释了早期地球磁场的偏差.
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
- 古磁论是古磁论的一种学说.
背景情况:
- 地心轴性双极 (GAD) 假设是古磁论的核心,它认为地球的磁场是一个与其轴对齐的中心双极.
- 在过去的1亿年里,GAD得到了很好的支持,但可能不会准确地描述比2亿5千万年前更早的场景.
- 以前的理论表明,较小的内核可能解释了早期的GAD偏差.
研究的目的:
- 为了调查地球早期磁场的GAD假设的有效性.
- 测试内核大小和内核-地幔边界热流变化对磁场的影响.
主要方法:
- 利用数值地力学模型来模拟地球的磁场.
- 模拟内核的大小各不相同.
- 在核心-地幔边界引入了可信的热流变化.
主要成果:
- 缩小内核大小对磁场的特征产生了微不足道的影响.
- 模拟的热流变化,与前中原时期的条件一致,诱导了显著的八极元件.
- 这种八极贡献挑战了早期地球的简单GAD模型.
结论:
- 内核大小不太可能是地球早期历史中GAD假设崩的主要原因.
- 核心-地幔边界的热流变化为GAD模型偏差提供了更合理的解释.
- 这些发现需要对中生时代前时期的古磁数据进行修订的解释.
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