ГЕОМОРФОЛОГИЯ И МОРФОТЕКТОНИКА ЛЕНО-АНГАРСКОГО ПЛАТО

dc.contributor.author	Уфимцев Г.Ф.
dc.contributor.author	Щетников А.А.
dc.contributor.author	Мяктова В.В.
dc.contributor.author	Филинов И.А.
dc.date.accessioned	2022-12-03T09:10:06Z
dc.date.available	2022-12-03T09:10:06Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=9142775
dc.identifier.citation	Геоморфология, 2005, , 2, 97-106
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/40706
dc.description.abstract	Lena-Angara plateau occupies the central part of the southern projection of Siberian platform. The young uplift of plateau has non-arched character. Its cause is the accretion of layered rock masses of platform cover, detached sub-horizontally by evaporates layers. Typta-Tutur depression has a peculiar position in the young tectonics of plateau, being the reversed-straighl morphostucture.
dc.title	ГЕОМОРФОЛОГИЯ И МОРФОТЕКТОНИКА ЛЕНО-АНГАРСКОГО ПЛАТО
dc.type	Статья
dc.subject.udc	551.4.033(235.3)

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