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塔拉绍德:修订间差异

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[[image:Korolev.png|thumb|right|250px|[[科罗廖夫环形山]]是一座典型的塔拉绍德结构示例<ref name=Shevchenko_2014/>]]
[[image:Korolev.png|thumb|right|250px|[[科罗廖夫环形山]]是一座典型的塔拉绍德结构示例<ref name=Shevchenko_2014/>]]


'''塔拉绍德'''<ref name=AES_2003/>([[英语]]:"Thalassoid";[[俄语]]:{{lang|ru|талассоид}}), 引自[[希腊语]]:“{{lang|el|θάλασσα}}”(海)和"{{lang|el|εἶδος}}"(外观),是[[月球]]上一种大小与[[月海]][[撞击盆地|盆地]]相类似的大型撞击结构<ref name=glossary_2005/><ref name=BSE/><ref name=Mosher_1970/>,但不同的是它有一个明亮的坑底,里面没有或仅覆盖了少量幽暗的[[熔岩]]。塔拉绍德底部及周边也散布有较小的[[陨石坑]],[[满月]]时,它与周边背景地形没有区别<ref name=Shevchenko_1980/>。
'''塔拉绍德'''<ref name=AES_2003/>([[英语]]:Thalassoid";[[俄语]]:{{lang|ru|талассоид}}), 引自[[希腊语]]:“{{lang|el|θάλασσα}}”(海)和{{lang|el|εἶδος}}(外观),是[[月球]]上一种大小与[[月海]][[撞击盆地|盆地]]相类似的大型撞击结构<ref name=glossary_2005/><ref name=BSE/><ref name=Mosher_1970/>,但不同的是它有一个明亮的坑底,里面没有或仅覆盖了少量幽暗的[[熔岩]]。塔拉绍德底部及周边也散布有较小的[[陨石坑]],[[满月]]时,它与周边背景地形没有区别<ref name=Shevchenko_1980/>。


塔拉绍德主要是[[月球背面]]的一种特征<ref name=Bakulin_1977/>,里面涌出的熔岩较正面的盆地要少得多,月背的塔拉绍德主要包含有[[智海 (月海)|智海]]、[[莫斯科海 (月球)|莫斯科海]]、[[东方海]]和[[赫茨普龙环形山]]、[[科罗廖夫环形山]]<ref name=Shevchenko_1980/>以及[[月球正面]]的[[神酒海|酒海]]<ref name=glossary_2005/><ref name=Shevchenko_1980/>。
塔拉绍德主要是[[月球背面]]的一种特征<ref name=Bakulin_1977/>,里面涌出的熔岩较正面的盆地要少得多,月背的塔拉绍德主要包含有[[智海 (月海)|智海]]、[[莫斯科海 (月球)|莫斯科海]]、[[东方海]]和[[赫茨普龙环形山]]、[[科罗廖夫环形山]]<ref name=Shevchenko_1980/>以及[[月球正面]]的[[神酒海|酒海]]<ref name=glossary_2005/><ref name=Shevchenko_1980/>。


==术语来历==
==术语来历==
该术语是[[前苏联]]在开始研究[[月球背面]]后提出的。1965年[[莫斯科国立大学]]教授尤里·帕夫洛维奇·普斯科夫<ref name=Maksimenko/><ref name=Shevchenko_2014/>在研究了当年[[探测器号系列探测器|探测器3号]]拍摄的照片后<ref name=Hartmann_1981/><ref name=Shevchenko_2014/>,将这一名词引入业内<ref name=Lipsky_1965/>。1967年,在[[国际天文学联合会]]第十三届大会上,苏联提请将该词列入月表特征[[行星体系命名法|命名]]通用术语集中,但遭拒绝。因而,该术语只作为一种对象特征,而非专用名<ref name=Proceedings_1967/><ref name=Shevchenko_2014/>。
该术语是[[前苏联]]在开始研究[[月球背面]]后提出的。1965年[[莫斯科国立大学]]教授尤里·帕夫洛维奇·普斯科夫<ref name=Shevchenko_2014/><ref name=Maksimenko/>在研究了当年[[探测器号系列探测器|探测器3号]]拍摄的照片后<ref name=Shevchenko_2014/><ref name=Hartmann_1981/>,将这一名词引入业内<ref name=Lipsky_1965/>。1967年,在[[国际天文学联合会]]第十三届大会上,苏联提请将该词列入月表特征[[行星体系命名法|命名]]通用术语集中,但遭拒绝。因而,该术语只作为一种对象特征,而非专用名<ref name=Shevchenko_2014/><ref name=Proceedings_1967/>。


西方国家不习惯塔拉绍德这一概念及相应术语,他们并不区分这些对象的种类,而只简单地统称为盆地<ref name=Wilhelms_1993_back/><ref name=Wilhelms_1993_notes/>。现在"塔拉绍德"这一概念已很少使用<ref name=Rodionova_1995/><ref name=Shevchenko_2014/>,如果它被接受,将有助于了解[[月海]]([[熔岩]]平原)和[[撞击盆地|盆地]]之间的差异<ref name=Shevchenko_2014/><ref name=Hartmann_1981/>。
西方国家不习惯塔拉绍德这一概念及相应术语,他们并不区分这些对象的种类,而只简单地统称为盆地<ref name=Wilhelms_1993_back/><ref name=Wilhelms_1993_notes/>。现在塔拉绍德这一概念已很少使用<ref name=Shevchenko_2014/><ref name=Rodionova_1995/>,如果它被接受,将有助于了解[[月海]]([[熔岩]]平原)和[[撞击盆地|盆地]]之间的差异<ref name=Shevchenko_2014/><ref name=Hartmann_1981/>。


==参考资料==
==参考资料==
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}}</ref>
}}</ref>
<ref name= BSE>[http://slovari.yandex.ru/~книги/БСЭ/Талассоид|title= Талассоид]</ref>
<ref name=BSE>[http://slovari.yandex.ru/~книги/БСЭ/Талассоид|title= Талассоид]{{Dead link|date=2018年7月 |bot=InternetArchiveBot |fix-attempted=no }}</ref>
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|journal=Multi-ring basins: Formation and evolution; Proceedings of the Lunar and Planetary Science Conference, Houston, TX, November 10-12, 1980. (A82-39033 19-91)
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|dead-url = no
}}</ref>
}}</ref>
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|author =Lipsky, Y. N.
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|title =Zond-3 Photographs of the Moon's Far Side
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|date =1965
|date =1965
|journal=Sky and Telescope
|journal=Sky and Telescope
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|bibcode=1965S&T....30..338L
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}}</ref>
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<ref name=Maksimenko>{{cite book
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}}</ref>
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}}</ref>
}}</ref>
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|publisher = The-Moon Wiki
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|accessdate = 2014-11-22
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|archiveurl = https://web.archive.org/web/20130925170453/http://the-moon.wikispaces.com/IAU+Transactions+XIIIB
|archivedate =2013-09-25
|archivedate = 2013-09-25
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}}</ref>
}}</ref>
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}}</ref>
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|author = Shevchenko V. V.
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|publisher = Springer New York
|date =2014
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|pages =1–2
|pages = 1–2
|isbn =978-1-4614-9213-9
|isbn = 978-1-4614-9213-9
|doi =10.1007/978-1-4614-9213-9_367-1
|doi = 10.1007/978-1-4614-9213-9_367-1
|url =http://link.springer.com/book/10.1007/978-1-4614-9213-9
|url = http://link.springer.com/book/10.1007/978-1-4614-9213-9
|chapterurl =http://link.springer.com/referenceworkentry/10.1007/978-1-4614-9213-9_367-1
|chapterurl = http://link.springer.com/referenceworkentry/10.1007/978-1-4614-9213-9_367-1
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|title = Легко ли достать Луну с неба?
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|journal =Звездочёт
|journal = Звездочёт
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|pages =8–11
|pages = 8–11
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|deadurl =no
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|article = Chapter 6. Back at the Main Event. 1965
|publisher =The University of Arizona Press
|publisher = The University of Arizona Press
|date =1993
|date = 1993
|pages =120
|pages = 120
|isbn =0-8165-1065-2
|isbn = 0-8165-1065-2
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|url = http://www.lpi.usra.edu/publications/books/rockyMoon
|chapterurl =http://www.lpi.usra.edu/publications/books/rockyMoon/07Chapter6.pdf
|chapterurl = http://www.lpi.usra.edu/publications/books/rockyMoon/07Chapter6.pdf
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|archive-date = 2020-12-31
|archive-url = https://web.archive.org/web/20201231213524/https://www.lpi.usra.edu/publications/books/rockyMoon/
|dead-url = no
}}</ref>
}}</ref>
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<ref name=Wilhelms_1993_notes>{{cite book
|title =To a Rocky Moon
|title = To a Rocky Moon
|author =Wilhelms D. E.
|author = Wilhelms D. E.
|article =Notes to pages 119–124
|article = Notes to pages 119–124
|publisher =The University of Arizona Press
|publisher = The University of Arizona Press
|date =1993
|date = 1993
|pages =394 (note 29)
|pages = 394 (note 29)
|isbn =0-8165-1065-2
|isbn = 0-8165-1065-2
|url =http://www.lpi.usra.edu/publications/books/rockyMoon
|url = http://www.lpi.usra.edu/publications/books/rockyMoon
|chapterurl =http://www.lpi.usra.edu/publications/books/rockyMoon/21Notes.pdf
|chapterurl = http://www.lpi.usra.edu/publications/books/rockyMoon/21Notes.pdf
|access-date = 2017-08-27
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|archive-url = https://web.archive.org/web/20201231213524/https://www.lpi.usra.edu/publications/books/rockyMoon/
|dead-url = no
}}</ref>
}}</ref>
}}
}}

2023年10月18日 (三) 10:34的最新版本

科罗廖夫环形山是一座典型的塔拉绍德结构示例[1]

塔拉绍德[2]英语:Thalassoid";俄语талассоид), 引自希腊语:“θάλασσα”(海)和εἶδος(外观),是月球上一种大小与月海盆地相类似的大型撞击结构[3][4][5],但不同的是它有一个明亮的坑底,里面没有或仅覆盖了少量幽暗的熔岩。塔拉绍德底部及周边也散布有较小的陨石坑满月时,它与周边背景地形没有区别[6]

塔拉绍德主要是月球背面的一种特征[7],里面涌出的熔岩较正面的盆地要少得多,月背的塔拉绍德主要包含有智海莫斯科海东方海赫茨普龙环形山科罗廖夫环形山[6]以及月球正面酒海[3][6]

术语来历

[编辑]

该术语是前苏联在开始研究月球背面后提出的。1965年莫斯科国立大学教授尤里·帕夫洛维奇·普斯科夫[1][8]在研究了当年探测器3号拍摄的照片后[1][9],将这一名词引入业内[10]。1967年,在国际天文学联合会第十三届大会上,苏联提请将该词列入月表特征命名通用术语集中,但遭拒绝。因而,该术语只作为一种对象特征,而非专用名[1][11]

西方国家不习惯塔拉绍德这一概念及相应术语,他们并不区分这些对象的种类,而只简单地统称为盆地[12][13]。现在塔拉绍德这一概念已很少使用[1][14],如果它被接受,将有助于了解月海熔岩平原)和盆地之间的差异[1][9]

参考资料

[编辑]
  1. ^ 1.0 1.1 1.2 1.3 1.4 1.5 Shevchenko V. V. http://link.springer.com/referenceworkentry/10.1007/978-1-4614-9213-9_367-1 |chapterurl=缺少标题 (帮助). Encyclopedia of Planetary Landforms. Springer New York. 2014: 1–2 [2017-08-27]. ISBN 978-1-4614-9213-9. doi:10.1007/978-1-4614-9213-9_367-1. (原始内容存档于2015-01-01).  |article=被忽略 (帮助)
  2. ^ https://web.archive.org/web/20150924015659/http://www.franko.lviv.ua/publish/astro/bukvy/t.pdf |archiveurl=缺少标题 (帮助) (PDF). Астрономічний енциклопедичний словник. Львів: ЛНУ—ГАО НАНУ. 2003: 468. ISBN 966-613-263-X. (原始内容 (PDF)存档于2015-09-24).  |article=被忽略 (帮助)
  3. ^ 3.0 3.1 Glossary of Geology 5. Springer Science & Business Media. 2005: 665. ISBN 978-0-922-15276-6. 
  4. ^ Талассоид[永久失效連結]
  5. ^ Mosher J. Lunar Farside Cratering (submitted in partial fulfilment of the requirements for the degree of bachelor of science) (PDF). Massachusets Institute of Technology. 1970: 10. (原始内容 (PDF)存档于2014-09-05). 
  6. ^ 6.0 6.1 6.2 Шевченко В. В. Современная селенография. М.: Наука. 1980: 51, 62–63. 
  7. ^ Бакулин П. И., Кононович Э. В., Мороз В. И. Курс общей астрономии 4. М.: Наука. 1977: 332. 
  8. ^ Максименко А. В. http://web.archive.org/web/20070617185041/astro.websib.ru/istor/23/Glava23.htm |chapterurl=缺少标题 (帮助). История астрономии в датах и именах. (原始内容存档于2007-06-17).  |article=被忽略 (帮助)
  9. ^ 9.0 9.1 Hartmann, W. K. Discovery of multi-ring basins: Gestalt perception in planetary science. Multi-ring basins: Formation and evolution; Proceedings of the Lunar and Planetary Science Conference, Houston, TX, November 10-12, 1980. (A82-39033 19-91). 1981: 79–90 [2017-08-27]. Bibcode:1981mrbf.conf...79H. (原始内容存档于2019-01-28). 
  10. ^ Lipsky, Y. N. Zond-3 Photographs of the Moon's Far Side. Sky and Telescope. 1965, 30: 338–341. Bibcode:1965S&T....30..338L. 
  11. ^ Proceedings of the Thirteenth General Assembly (Prague, 1967) – excerpts. The-Moon Wiki. [2014-11-22]. (原始内容存档于2013-09-25). 
  12. ^ Wilhelms D. E. http://www.lpi.usra.edu/publications/books/rockyMoon/07Chapter6.pdf |chapterurl=缺少标题 (帮助) (PDF). To a Rocky Moon. The University of Arizona Press. 1993: 120 [2017-08-27]. ISBN 0-8165-1065-2. (原始内容存档于2020-12-31).  |article=被忽略 (帮助)
  13. ^ Wilhelms D. E. http://www.lpi.usra.edu/publications/books/rockyMoon/21Notes.pdf |chapterurl=缺少标题 (帮助) (PDF). To a Rocky Moon. The University of Arizona Press. 1993: 394 (note 29) [2017-08-27]. ISBN 0-8165-1065-2. (原始内容存档于2020-12-31).  |article=被忽略 (帮助)
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