| Form of presentation | Articles in Russian journals and collections |
| Year of publication | 2022 |
| Язык | русский |
|
Shpekin Mikhail Ivanovich, author
|
|
Barenbaum Azariy Aleksandrovich, author
|
| Bibliographic description in the original language |
Barenbaum AA, Shpekin M I. On origin and age of Orientale basin on Moon // Experiment in Geosciences. 2022.V.28, No1, 5-8.
|
| Annotation |
The Oriental Basin is considered to be the youngest multi-ring impact basin on the Moon. The basin age,
however, is unknown and its determination is a very
difficult problem. In this article we concluded that the Orientale Basin was
formed about ~1 Ma during the last bombardment of Moon
by galactic comets of the Orion-Cygnus jet stream. To
substantiate this conclusion, we used measurements of
comet flux density in this jet stream, invoked a new
explanation of the giant South Pole–Aitken Basin origin by
galactic comets, as well as analyzed the distribution density of large craters in floor of Orientale Basin.
|
| Keywords |
Orientale and South Pole-Aitken basins on
Moon, galactic comets of Orion-Cygnus jet stream
|
| The name of the journal |
Experiment in Geosciences
|
| URL |
http://www.iem.ac.ru/experiment/pdf/2022/p1.pdf |
| Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=272240&p_lang=2 |
Full metadata record  |
| Field DC |
Value |
Language |
| dc.contributor.author |
Shpekin Mikhail Ivanovich |
ru_RU |
| dc.contributor.author |
Barenbaum Azariy Aleksandrovich |
ru_RU |
| dc.date.accessioned |
2022-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2022-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2022 |
ru_RU |
| dc.identifier.citation |
Barenbaum AA, Shpekin M I. On origin and age of Orientale basin on Moon // Experiment in Geosciences. 2022.V.28, No1, 5-8.
|
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=272240&p_lang=2 |
ru_RU |
| dc.description.abstract |
Experiment in Geosciences |
ru_RU |
| dc.description.abstract |
The Oriental Basin is considered to be the youngest multi-ring impact basin on the Moon. The basin age,
however, is unknown and its determination is a very
difficult problem. In this article we concluded that the Orientale Basin was
formed about ~1 Ma during the last bombardment of Moon
by galactic comets of the Orion-Cygnus jet stream. To
substantiate this conclusion, we used measurements of
comet flux density in this jet stream, invoked a new
explanation of the giant South Pole–Aitken Basin origin by
galactic comets, as well as analyzed the distribution density of large craters in floor of Orientale Basin.
|
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
Orientale and South Pole-Aitken basins on
Moon |
ru_RU |
| dc.subject |
galactic comets of Orion-Cygnus jet stream
|
ru_RU |
| dc.title |
On origin and age of Orientale basin on Moon |
ru_RU |
| dc.type |
Articles in Russian journals and collections |
ru_RU |
|
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