TO PROBLEM OF PLEISTOCENE HISTORY OF FORMING OF VALLEY RELIEF ON LEFT BANK OF THE MIDDLE DNIEPER. Paper 1. System-geomorphological sights of two glacial transgressive stages
According to the features of the geomorphological structure of the valley of the middle Dnieper, some episodes of its Neo-Pleistocene history have been reconstructed.Presence of morphosedimentic signs of two glaciations at this area is shown
Збережено в:
| Дата: | 2018 |
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| Автор: | |
| Формат: | Стаття |
| Мова: | Ukrainian |
| Опубліковано: |
Institute of Geological Sciences, NAS of Ukraine
2018
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| Теми: | |
| Онлайн доступ: | http://geojournal.igs-nas.org.ua/article/view/133459 |
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| Назва журналу: | Geological journal |
Репозитарії
Geological journal| Резюме: | According to the features of the geomorphological structure of the valley of the middle Dnieper, some episodes of its Neo-Pleistocene history have been reconstructed.Presence of morphosedimentic signs of two glaciations at this area is shown |
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