КАРСТОВАЯ ДЕНУДАЦИЯ НА ТЕРРИТОРИИ СИБИРИ И ДАЛЬНЕГО ВОСТОКА: ОСОБЕННОСТИ СОВРЕМЕННОГО РАЗВИТИЯ

dc.contributor.author	Трофимова Е.В.
dc.date.accessioned	2024-04-06T00:47:25Z
dc.date.available	2024-04-06T00:47:25Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=9433392
dc.identifier.citation	Геоморфология, 2006, , 3, 78-84
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/43383
dc.description.abstract	Using he methods of J. Corbel and M. Pulina the estimation of a karstic denudation was accomplished for 127 river valleys of the Siberia and the Far East. Its magnitude varies from 1.1 to 62.0 mm/millennium within the region explored. The climatic conditions, especially precipitation, play the main role in the development of the karst. The intensity of karstic process has been revealed to differ in river basins with permafrost from that in the basins without permafrost.
dc.title	КАРСТОВАЯ ДЕНУДАЦИЯ НА ТЕРРИТОРИИ СИБИРИ И ДАЛЬНЕГО ВОСТОКА: ОСОБЕННОСТИ СОВРЕМЕННОГО РАЗВИТИЯ
dc.type	Статья
dc.subject.udc	551.435.8(571)

Files in this item

Files	Size	Format	View
There are no files associated with this item.