FENNOSCANDIAN AND SARMATIAN SEGMENTS OF THE EAST EUROPEAN PLATFORM
R.G. Garetsky and G.I. Karatayev
Institute of Environmental Sciences of Belarus, ul. F. Skoryny 10, Minsk, 220114, Belarus
Keywords: Seismic gravity modeling, suture zone, subduction, collision, geotransect, East European Platform
Pages: 1228-1235
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 result 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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