КФУ. Карточка публикации. On origin and age of Orientale basin on Moon

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ON ORIGIN AND AGE OF ORIENTALE BASIN ON MOON

Форма представления

Статьи в российских журналах и сборниках

Год публикации

2022

Язык

русский

Авторы, сотрудники КФУ

Шпекин Михаил Иванович, автор

Другие авторы

Баренбаум Азарий Александрович, автор

Библиографическое описание на языке оригинала

Barenbaum AA, Shpekin M I. On origin and age of Orientale basin on Moon // Experiment in Geosciences. 2022.V.28, No1, 5-8.

Аннотация

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.

Ключевые слова

Orientale and South Pole-Aitken basins on Moon, galactic comets of Orion-Cygnus jet stream

Название журнала

Experiment in Geosciences

URL

http://www.iem.ac.ru/experiment/pdf/2022/p1.pdf

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https://repository.kpfu.ru/?p_id=272240

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Шпекин Михаил Иванович	ru_RU
dc.contributor.author	Баренбаум Азарий Александрович	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/?p_id=272240	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	Статьи в российских журналах и сборниках	ru_RU