相关实验视频
Updated: May 16, 2026

06:14
Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
Published on: July 30, 2020
由GRAIL看到的月球地
Mark A Wieczorek1, Gregory A Neumann, Francis Nimmo
1Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, Case 7071, Lamarck A, 5, rue Thomas Mann, 75205 Paris Cedex 13, France. wieczor@ipgp.fr
概括
月亮的月亮的月亮
科学领域:
- 月球地质学 月球地质学
- 星球地质物理学 星球地质物理学
背景情况:
- 关于月球高地地层密度的先前假设.
- 需要准确的地模型.
研究的目的:
- 为了确定月球高地地的大量密度和多孔性.
- 为了将毛孔度和密度的变化与地质特征和组成相关联.
- 开发一个全球地厚度模型.
主要方法:
- 来自重力恢复和内部实验室 (GRAIL) 航天器的高分辨率重力数据的分析.
- 遥感和月球样本数据的整合.
- 与阿波罗的地震约束情况进行比较.
主要成果:
- 月球高地地的散装密度为2550公斤/立方米,低于之前的假设.
- 这意味着在几公里深处,地的平均孔隙率为12%.
- 孔径与冲击盆相关;密度与组成相关.
- 全球地厚度模型 (3443公里) 与这些发现一致.
结论:
- 月球的高地地比以前认为的要多孔得多.
- 低地密度支持全球厚度模型,并表明与地球相比,月球组成不一定富含耐火元素.
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