ЭВОЛЮЦИЯ СКЛОНОВ ДОЛИН НИЗШИХ ПОРЯДКОВ НА ОСНОВЕ ПРЕДСТАВЛЕНИЙ О ГЕОМОРФОЛОГИЧЕСКОЙ ФАЦИИ (НА ПРИМЕРЕ НИЗКОГОРЬЯ ЮЖНОГО СИХОТЭ-АЛИНЯ)
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Невский В.Н. | |
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=9213569 | |
dc.identifier.citation | Геоморфология, 2006, , 2, 101-109 | |
dc.identifier.issn | 0435-4281 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/42940 | |
dc.description.abstract | Geomorphologic facie of slopes is specified by two independent parameters: the steepness of the slope and mechanical composition of deposit (or characteristic of denuded slope surface). Using this idea author represents the scheme of mountain relief flattening under the condition of rhythmic fluvial activity. According to idealized scheme the slope evolution is directional discontinuous process, of which every episode includes denudation and accumulative stages. In the reality they may be not strictly separated. | |
dc.title | ЭВОЛЮЦИЯ СКЛОНОВ ДОЛИН НИЗШИХ ПОРЯДКОВ НА ОСНОВЕ ПРЕДСТАВЛЕНИЙ О ГЕОМОРФОЛОГИЧЕСКОЙ ФАЦИИ (НА ПРИМЕРЕ НИЗКОГОРЬЯ ЮЖНОГО СИХОТЭ-АЛИНЯ) | |
dc.type | Статья | |
dc.subject.udc | 551.4.037(235.47) |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru