ОСНОВНЫЕ ЭТАПЫ ИСТОРИИ РЕЧНЫХ ДОЛИН ЦЕНТРА РУССКОЙ РАВНИНЫ В ПОЗДНЕМ ВАЛДАЕ И ГОЛОЦЕНЕ: РЕЗУЛЬТАТЫ ИССЛЕДОВАНИЙ В СРЕДНЕМ ТЕЧЕНИИ Р. СЕЙМ
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dc.contributor.author | Панин А.В. | |
dc.contributor.author | Сидорчук А.Ю. | |
dc.contributor.author | Баслеров С.В. | |
dc.contributor.author | Борисова О.К. | |
dc.contributor.author | Ковалюх Н.Н. | |
dc.contributor.author | Шеремецкая Е.Д. | |
dc.date.accessioned | 2021-03-23T04:31:48Z | |
dc.date.available | 2021-03-23T04:31:48Z | |
dc.date.issued | 2001 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14997878 | |
dc.identifier.citation | Геоморфология, 2001, , 2, 19-34 | |
dc.identifier.issn | 0435-4281 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/27058 | |
dc.description.abstract | The main fluvial development stages of the Russian Plain have been revealed. The result is based on the investigations of landforms and deposits of low terraces, flood-plains and river channels of Seim and Svapa rivers. These stages are: 1) 17-19 Ma B.P. - formation of constrative alluvium layers of sand and siltstone more than 10 m thick; 2) 14-17 Ma - formation of the large meandering river channels with discharge 6-7 times more and normal alluvium thick 1.5-2 times more than recent; 3) 10-14 Ma - the reduction of large channels and formation of inherited flood-plains and its deposits; 4) less than 10 Ma - formation of recent meandering river channels and the belt of segment-ridges flood-plain under the conditions of long-period changes of water discharge. | |
dc.subject | Голоцен | ru |
dc.title | ОСНОВНЫЕ ЭТАПЫ ИСТОРИИ РЕЧНЫХ ДОЛИН ЦЕНТРА РУССКОЙ РАВНИНЫ В ПОЗДНЕМ ВАЛДАЕ И ГОЛОЦЕНЕ: РЕЗУЛЬТАТЫ ИССЛЕДОВАНИЙ В СРЕДНЕМ ТЕЧЕНИИ Р. СЕЙМ | |
dc.type | Статья | |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | ru |
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