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月球地幔的热不对称性由每月的潮反应推断出来
R S Park1, A Berne2, A S Konopliv3
1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA. Ryan.S.Park@jpl.nasa.gov.
Nature
|May 14, 2025
概括
月亮
科学领域:
- 月球地质学
- 星球科学
- 固体地球地质学
背景情况:
- 月球的重力场因地球的潮力而发生变化.
- 这些变化对月球的内部结构很敏感.
- 之前的模型通常假定月球内部是对称的.
研究的目的:
- 使用太空飞船数据恢复月球时间变化的重力场.
- 为了确定3度的重力潮数 (k3).
- 根据潮反应调查月球的内部结构.
主要方法:
- 采用了美国宇航局的GRAIL飞船的数据.
- 恢复时间变化的月球重力场.
- 计算了3度的重力潮数 (k3).
主要成果:
- 估计的 k3 = 0.0163 ± 0.0007.
- 这个值比对称的月球高出72%.
- 一个大的k3表明地幔的弹性剪切模量有显著的变化.
结论:
- 月球的内部不是球形对称的.
- 证实了深层月球地幔的侧向异质性.
- 月球地质和地震性可能受到近侧地幔持续的热异常的影响.
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