Postglacial tectonics and palaeoseisic dislocation in the Kovda area (Kandalaksha Bay, eastern Fennoscandian Shield)

The Kandalaksha Graben of the White Sea is one of the most active tectonic zones of the eastern part of the Fennoscandian crystalline shield. Active faults of the Kandalaksha Graben derive from the axial zone of the Paleoproterozoic mobile Lapland Granulite Belt and the Riphean paleorift system. The...

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Bibliographic Details
Published in:Vestnik of Saint Petersburg University. Earth Sciences
Main Author: Nikolaeva, Svetlana B.
Format: Article in Journal/Newspaper
Language:Russian
Published: St Petersburg State University 2019
Subjects:
Online Access:https://doi.org/10.21638/spbu07.2019.304
http://hdl.handle.net/11701/16758