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Rayed craters on the far side of the Moon
https://doi.org/10.24517/00011142
https://doi.org/10.24517/000111420caa90dc-a745-42e9-b834-de15093ae60f
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
AA00835991-47-01_02-002.pdf (307.4 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2017-10-03 | |||||
| タイトル | ||||||
| タイトル | Rayed craters on the far side of the Moon | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 資源タイプ | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | departmental bulletin paper | |||||
| ID登録 | ||||||
| ID登録 | 10.24517/00011142 | |||||
| ID登録タイプ | JaLC | |||||
| 著者 |
Morota, Tomokatsu
× Morota, Tomokatsu× Furumoto, Muneyoshi |
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| 著者別表示 |
諸田, 智克
× 諸田, 智克× 古本, 宗充 |
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| 提供者所属 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Department of Earth Sciences, Faculty of Science, Kanazawa University | |||||
| 提供者所属 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | Department of Earth Sciences, Faculty of Science, Kanazawa University | |||||
| 書誌情報 |
The science reports of the Kanazawa University = 金沢大学理科報告 巻 47, 号 1-2, p. 49-58, 発行日 2003-01-01 |
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| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 0022-8338 | |||||
| その他の識別子 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | AA00835991 | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | A fresh crater on the Moon is associated with bright rays, which are made of fresh ejecta from the main and secondary craters. Rays of a lunar crater generally become indistinguishable from the background materials with the age, and the lifetime of a ray is supposed to be about 0.8 Gyr. Using Clementine 750-nm mosaic images, we identify rayed craters mainly on the far side of the Moon. A total of 235 rayed craters which are larger than 5 km in diameter are identified in an area of about 1.55 x 10^7 km^2. The size-frequency distribution for the rayed craters indicates a lack of small rayed craters, implying that the preservation of ray depends on the crater size. | |||||
