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Updated: May 16, 2026

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Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
Published on: July 30, 2020
GRAILから見た月の地殻
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
まとめ
月は月,月が月である.
科学分野:
- 月面地質学 月面地質学
- 惑星の地球物理学
背景:
- 月面の高原の地殻密度に関する以前の仮定.
- 正確な地殻モデルが必要である.
研究 の 目的:
- 月の高地地地殻の質量密度と多孔性を決定するために.
- 毛細さと密度の変動を地質学的特徴と組成と相関させるため.
- グローバルな地殻の厚さモデルを開発する.
主な方法:
- グラビティ・リカバリー・アンド・インテリア・ラボラトリー (GRAIL) の宇宙船からの高解像度重力データの分析.
- リモートセンシングと月のサンプルデータの統合.
- アポロの地震制約との比較.
主要な成果:
- 月の高地地地殻の質量密度は2550kg/m3で,これまで考えられていたよりも低い.
- これは,数キロメートルの深さまで,平均12%の地殻の多孔性を意味する.
- 毛細さは衝突盆と相関し,密度は組成と相関する.
- グローバルな地殻厚さモデル (3443 km) は,これらの発見と一致しています.
結論:
- 月の高原の地殻は,これまで考えられていたよりもかなり多孔性がある.
- 低地殻密度は,地球厚さのモデルを支持し,月面の構成は,地球と比較して,必ずしも耐火性元素で豊かにされていないことを示唆しています.
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