ДЕПРЕССИИ СНЕГОВЫХ ГРАНИЦ ПЛЕЙСТОЦЕНОВЫХ ОЛЕДЕНЕНИЙ ВОСТОЧНОГО ЗАБАЙКАЛЬЯ

dc.contributor.author	Еникеев Ф.И.
dc.date.accessioned	2024-04-05T23:52:48Z
dc.date.available	2024-04-05T23:52:48Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9433390
dc.identifier.citation	Геоморфология, 2006, , 3, 56-65
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/43371
dc.description.abstract	The localization of the climatic and orographic snowlines during the Late Pleistocene glaciations was determined for the southern part of the East Siberia: Vitim-Olekma watershed and Eastern Transbaikalia. The deformation of the snowlines depends on global, regional, and local agents. Depression of the chionosphere reached 1400 m in the Sar-tan Ice Age, 1600 m - in the Muruktin, 1800 m - in the Tas stages, and more than 1900 - in the Samarovo Ice Age.
dc.title	ДЕПРЕССИИ СНЕГОВЫХ ГРАНИЦ ПЛЕЙСТОЦЕНОВЫХ ОЛЕДЕНЕНИЙ ВОСТОЧНОГО ЗАБАЙКАЛЬЯ
dc.type	Статья
dc.subject.udc	551.435.4(-925.16)
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен

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