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...
Published in: | Vestnik of Saint Petersburg University. Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | Russian |
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St Petersburg State University
2019
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Online Access: | https://doi.org/10.21638/spbu07.2019.304 http://hdl.handle.net/11701/16758 |