Lithospheric structure of the western part of the East European Craton investigated by deep seismic profiles

The Palaeoproterozoic collision of Archaean Fennoscandia, Volgo-Uralia and Sarmatia, viewed as a large composite of terranes, each with an independent history during Archaean and Early Proterozoic time, formed the East European Craton. This paper summarizes the results of deep seismic sounding inves...

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Bibliographic Details
Main Authors: Jacyna, Juozas, Korabliova, Larisa, Motuza Matuzevičius, Gediminas, Nasedkin, Viktor, Šečkus, Rimantas
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:http://vu.lvb.lt/VU:ELABAPDB3664319&prefLang=en_US