РЕЛИКТЫ КЛИМАТОВ ГЕОЛОГИЧЕСКОГО ПРОШЛОГО В РЕЛЬЕФЕ ЕВРАЗИИ

dc.contributor.author	Дедков А.П.
dc.contributor.author	Тимофеев Д.А.
dc.contributor.author	Мозжерин В.В.
dc.contributor.author	Спасская И.И.
dc.date.accessioned	2021-12-07T03:40:52Z
dc.date.available	2021-12-07T03:40:52Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17349778
dc.identifier.citation	Геоморфология, 2003, , 1, 9-14
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/33000
dc.description.abstract	During the Meso-Cenozoic time, changes of climate resulted more than once in that exogenic morphogenesis types replaced one another and relief underwent restructuring. It should be noticed, however, that though new land-forms evolved in the process, some of older once persisted as relicts from former climates. There is a distinct zonality in distribution of relict landforms over plains of Europe.
dc.subject	Cenozoic
dc.title	РЕЛИКТЫ КЛИМАТОВ ГЕОЛОГИЧЕСКОГО ПРОШЛОГО В РЕЛЬЕФЕ ЕВРАЗИИ
dc.type	Статья
dc.subject.udc	551.4.072(4/5)
dc.subject.age	Cenozoic
dc.subject.age	Кайнозой	ru

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