geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2692Research ArticleНаучные сообщенияShort communicationsМорфотектоническое развитие северо-восточной части Балтийского щита в фанерозоеMorphotectonic evolution of the NE Baltic shield during the Phanerozoic timeРубинраутГ. С.RubinrautG. S.Геологический институт Кольского филиала АН СССРРоссия19871511202202Геоморфология9094Copyright © Рубинраут Г.С., 20222022Рубинраут Г.С.Rubinraut G.S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2692

Geodynamic conditions of the Kola Peninsula morphostructural features development are preconditioned by the Baltic shield beginning as an individual structural unit in Riphean and since then by unidirectional intermittent development of zones of the basement submergence and spreading at the south of the Barents Sea plate and within the White Sea graben as well as by the Scandinavian Caledonides geological history. These geodynamic conditions controlled the process and direction of the relief formation at the Kola Peninsula during the Phanerozoic.

Geodynamic conditions of the Kola Peninsula morphostructural features development are preconditioned by the Baltic shield beginning as an individual structural unit in Riphean and since then by unidirectional intermittent development of zones of the basement submergence and spreading at the south of the Barents Sea plate and within the White Sea graben as well as by the Scandinavian Caledonides geological history. These geodynamic conditions controlled the process and direction of the relief formation at the Kola Peninsula during the Phanerozoic.

References

The authors declare that there are no conflicts of interest present.