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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
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| Format: | Article |
| Language: | Ukrainian |
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Institute of Geological Sciences, NAS of Ukraine
2018
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| Online Access: | http://geojournal.igs-nas.org.ua/article/view/133459 |
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