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Crustal dichotomy and reorientation of the Moon as a consequence of a leading-trailing asymmetry in the cratering rate
https://jaxa.repo.nii.ac.jp/records/20579
https://jaxa.repo.nii.ac.jp/records/2057967958608-0a3d-4b88-b779-1c36ce736531
Item type | 会議発表論文 / Conference Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2015-03-26 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Crustal dichotomy and reorientation of the Moon as a consequence of a leading-trailing asymmetry in the cratering rate | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 月 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地殻2分 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 回転動力学 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 慣性モーメント | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 構造的水盤 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 月地殻厚さ | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | インパクター | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | クレーター形成 | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Moon | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | crustal dichotomy | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | rotational dynamics | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | moment of inertia | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | structural basin | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | lunar crustal thickness | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | impactor | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | cratering | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_5794 | |||||
資源タイプ | conference paper | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
その他のタイトル | ||||||
その他のタイトル | クレーター形成速度における先端部と尾部の非対称性の結果として月の地殻2分と再方位 | |||||
著者 |
諸田, 智克
× 諸田, 智克× 鵜飼, 啓之× 古本, 宗充× Morota, Tomokatsu× Ukai, Takashi× Furumoto, Muneyoshi |
|||||
著者所属 | ||||||
金沢大学 大学院自然科学研究科 | ||||||
著者所属 | ||||||
金沢大学 大学院自然科学研究科 | ||||||
著者所属 | ||||||
金沢大学 大学院自然科学研究科 | ||||||
著者所属(英) | ||||||
en | ||||||
Kanazawa University Graduate School of Natural Science and Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Kanazawa University Graduate School of Natural Science and Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Kanazawa University Graduate School of Natural Science and Technology | ||||||
出版者 | ||||||
出版者 | 宇宙航空研究開発機構宇宙科学研究本部 | |||||
出版者(英) | ||||||
出版者 | Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA/ISAS) | |||||
書誌情報 |
第37回月・惑星シンポジウム en : Proceedings of the 37th ISAS Lunar and Planetary Symposium p. 1-4, 発行日 2004-02 |
|||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Impacts on the early Moon are expected to have been extremely asymmetrical between the leading and trailing hemispheres because of a fast orbital motion of the Moon. In this paper, suggested is an influence of the heavy asymmetrical bombardment upon the rotational dynamics of the early Moon. The preferential bombardment thinned the crust of the leading hemisphere and thickened that of the trailing hemisphere. As a consequence of the redistribution of crustal materials, the axis of the minimum principal moment of inertia shifted toward the west. The Moon was reoriented eastwards with the new minimum axis along the Earth-Moon line. The sequential actions operated continuously and concurrently on the early Moon, so that the Moon was gradually rotated toward the east. Longitudinal distributions of impact basins and crustal thickness models support the scenario proposed here. | |||||
資料番号 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 資料番号: AA0047898001 |