Present article represents geologic-geomorphologic and structural features of Late Quaternary glacial-marine sediments in the northernmost part of Novaya Zemlya shelf. Upper regional unconformity (URU), Late Quaternary glacial complex bottom and exaration markers were plotted within the studied area.
How to cite:
Dorechkina , D. E., Rekant , P. V., Korshunov , D. A., & Portnov , A. D. (2012). The distribution of late quaternary glacial-marine deposite on the norternmost part оf Novaya Zemlya shelf. Journal of Mining Institute, 195, 33. Retrieved from https://pmi.spmi.ru/index.php/pmi/article/view/6095
