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...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2006
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Subjects: | |
Online Access: | http://vu.lvb.lt/VU:ELABAPDB3664319&prefLang=en_US |