Seismites resulting from high-frequency, high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift

Geologically extremely rapid changes in altitude by glacial rebound of the Earth crust after retreat of the Scandinavian Ice Sheet at the end of the last Weichselian glaciation influenced the palaeogeography of northern Europe. The uplift of the Earth crust apparently was not gradual, but shock-wise...

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Detalles Bibliográficos

Principais autores:	A.J. (Tom) van Loon, Małgorzata Pisarska-Jamroży, Māris Nartišs, Māris Krievāns, Juris Soms
Formato:	Artigo
Idioma:	Inglês
Publicado:	Elsevier 2016-09-01
Series:	Journal of Palaeogeography
Assuntos:	Soft-sediment deformation structures (SSDS), Seismites Latvia Glacio-isostatic rebound Earthquake recurrence time
Acceso en liña:	http://www.sciencedirect.com/science/article/pii/S2095383616300220
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