О СООТНОШЕНИИ СКОРОСТЕЙ СОВРЕМЕННОЙ ДЕНУДАЦИИ И ТЕКТОНИЧЕСКИХ ПОДНЯТИЙ ЭПИГЕОСИНКЛИНАЛЬНЫХ ГОР ЕВРАЗИИ

dc.contributor.author	Мамина Л.Р.
dc.date.accessioned	2022-12-15T08:23:31Z
dc.date.available	2022-12-15T08:23:31Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=9148988
dc.identifier.citation	Геоморфология, 2005, , 3, 98-101
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/40930
dc.description.abstract	Recent mechanical denudation rate in Alps, Carpathians, West and East Caucasus, and Himalayas was estimated by the sediment discharge data. The values obtained were compared with tectonic uplift velocities. Everywhere within the axial zone of the mountains the tectonic uplift predominates denudation in ratio 1.8:1 - 6.4:1. This indicates the continuous upward evolution of mountains. Recent rates of mountains uplift are higher than average rates for the whole neotectonic stage.
dc.title	О СООТНОШЕНИИ СКОРОСТЕЙ СОВРЕМЕННОЙ ДЕНУДАЦИИ И ТЕКТОНИЧЕСКИХ ПОДНЯТИЙ ЭПИГЕОСИНКЛИНАЛЬНЫХ ГОР ЕВРАЗИИ
dc.type	Статья
dc.subject.udc	551.432(-924/-925)

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