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Subsea uplifts origin of the Rugozerskaya Bay and the Great Salma channel (Kandalaksha Bay)статья
Статья опубликована в журнале из списка Web of Science и/или Scopus
- Авторы: Terekhina Y.E., Tokarev M.Y., Kozupitsa N.A., Shevchenko N.V.
- Журнал: Moscow University Geology Bulletin
- Том: 72
- Номер: 3
- Год издания: 2017
- Издательство: Allerton Press Inc.
- Местоположение издательства: United States
- Первая страница: 209
- Последняя страница: 214
- Аннотация: The origin of the subsea uplifts of the Rugozerskaya bay and the Great Salma strait is discussed in this article. It was found that the present-day bottom surface of the investigation area imitates the post-glacial terrain. This was determined by accumulative glacial formations that were emulated with post-glacial sedimentation processes. All modern bottom uplifts are similar to the ancient post-glacial terrain. Most presentday bottom surface depressions are similar to post-glacial surface inequalities, but the configuration of modern closed kettles could be changed via glacial–marine sedimentation and other processes.
- Добавил в систему: Замотина Злата Сергеевна