TRACES OF SEISMIC ACTIVITY IN THE LAKE BOTTOM SEDIMENTS OF EASTERN FENNOSCANDIA

This paper presents the results of a study on traces of ancient earthquakes in the lake bottom sediments of eastern Fennoscandia (Kola region and Karelia). Based on the sediment cores from six lake basins located within large active structures of the region, consideration is being given to the most...

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Autore principale:	S. B. Nikolaeva
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2022-12-01
Serie:	Геодинамика и тектонофизика
Soggetti:	earthquake-induced deformation earthquake bottom sediment lake fault fennoscandian shield kola region karelia holocene
Accesso online:	https://www.gt-crust.ru/jour/article/view/1587
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