Publication Date:
2011-10-01
Description:
Seismic gravity modeling along the Eurobridge-96-Eurobridge-97 DSS geotransects has shown that the Central Belarus suture zone formed in the Paleoproterozoic as a results of the subduction and collision processes at the convergent junction of the Fennoscandian and Sarmatian segments of the East European Platform. The influence of pre-Riphean processes on the subsequent tectonic events occurring on the territory of Belarus during the Phanerozoic has been established. © 2011, V.S. Sobolev IGM, Siberian Branch of the RAS.
Print ISSN:
1068-7971
Electronic ISSN:
1878-030X
Topics:
Geosciences
,
Physics
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