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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Bibliographische Detailangaben
Datum:2018
1. Verfasser: Karpenko, A.
Format: Artikel
Sprache:Ukrainian
Veröffentlicht: Institute of Geological Sciences, NAS of Ukraine 2018
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Online Zugang:http://geojournal.igs-nas.org.ua/article/view/133459
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Назва журналу:Geological journal

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Geological journal