Russian Geology and Geophysics · 2011 · 11 citations · 3 references
Natural SciencesEarth SciencesGeologyMarine GeologyTectonicsTectonophysicsContinental RiftingMarine TectonicsPlate TectonicsRegional TectonicsRift StructuresTectonic GeomorphologyContinental TectonicsIntracontinental Rift SystemsRift EvolutionRift Segment LinkageRift SegmentationTectonic Boundary EvolutionTectonic StudiesTriple Junction Tectonics
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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