ЗАКОНОМЕРНОСТИ ФОРМИРОВАНИЯ ОБЛОМОЧНОГО МАТЕРИАЛА В ПРИУРЕЗОВОЙ ПОЛОСЕ ОЗЕРА БАЙКАЛ

dc.contributor.author	Потемкина Т.Г.
dc.date.accessioned	2024-03-09T07:07:18Z
dc.date.available	2024-03-09T07:07:18Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9213570
dc.identifier.citation	Геоморфология, 2006, , 2, 109-117
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42941
dc.description.abstract	The weakness of accumulation is the characteristic feature of the Baikal coastal zone. The coarse sediments are predominant at the water edge. The type of the coast depends on the structure of the lake basin. High rocky banks are typical for the west flange, where accumulation is almost absent. The east low-graded flange has much of an entass-ments, enrockments, and pebble beaches.
dc.title	ЗАКОНОМЕРНОСТИ ФОРМИРОВАНИЯ ОБЛОМОЧНОГО МАТЕРИАЛА В ПРИУРЕЗОВОЙ ПОЛОСЕ ОЗЕРА БАЙКАЛ
dc.type	Статья
dc.subject.udc	551.435.32(-925.16)

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