ГЕОМОРФОЛОГИЧЕСКИЙ ОЧЕРК ЮЖНОГО МАКРОСКЛОНА СТАНОВОГО ХРЕБТА
| dc.contributor.author | Ликутов Е.Ю. | |
| dc.date.accessioned | 2021-12-08T07:10:31Z | |
| dc.date.available | 2021-12-08T07:10:31Z | |
| dc.date.issued | 2003 | |
| dc.description.abstract | Special geomorphologic investigations were carried out at the southern slope of Stanovoi ridge. Slopes are shown to play the main role in the tructure and zoning of landforms; the stable slope associations of different dynamic types, an important role of tectonic tilts of land surface, self-development capability are the main features of the relief. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=17360971 | |
| dc.identifier.citation | Геоморфология, 2003, , 4, 72-87 | |
| dc.identifier.issn | 0435-4281 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/33099 | |
| dc.subject.udc | 551.4.035(235.34) | |
| dc.title | ГЕОМОРФОЛОГИЧЕСКИЙ ОЧЕРК ЮЖНОГО МАКРОСКЛОНА СТАНОВОГО ХРЕБТА | |
| dc.type | Статья |