| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4738594 | Russian Geology and Geophysics | 2011 | 8 Pages |
Abstract
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.
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