ВОДОСБОРНЫЕ ВОРОНКИ (ЦИРКИ) СИХОТЭ-АЛИНЯ И ЧЕРНОГОРЬЯ (ПРИМОРСКИЙ КРАЙ)

dc.contributor.author	Короткий А.М.
dc.date.accessioned	2021-12-08T07:10:31Z
dc.date.available	2021-12-08T07:10:31Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17357098
dc.identifier.citation	Геоморфология, 2003, , 2, 76-88
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/33089
dc.description.abstract	The description of the morphology of catchment funnels and their distribution within the Sikhote-Alin and Chernogorie is given. These landforms are considered as independent elements of geomorphological zoning in the upper parts of any catchment basin. The main features of quaternary deposits (lithocomplexes) correlated to catchment funnels are considered. Their formation proved to be durable and effected by denudation intensity changes caused by tectonic and climate. The characteristics were determined, which make it possible to distinguish clacial circus from catchment funnels.
dc.subject	Quaternary
dc.title	ВОДОСБОРНЫЕ ВОРОНКИ (ЦИРКИ) СИХОТЭ-АЛИНЯ И ЧЕРНОГОРЬЯ (ПРИМОРСКИЙ КРАЙ)
dc.type	Статья
dc.subject.udc	551.435.164(571.63)
dc.subject.age	Cenozoic::Quaternary
dc.subject.age	Кайнозой::Четвертичная	ru

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