New geochemical data on Holocene pedorelics in Belarus are presented. Some problems of the soilmantle evolution during the Holocene and the peculiarities of the paleosoils, especially buried flood-plain soils of the Nieman, Dnieper and Pripyat valleys are discussed. Arkhipova A.A., Naidenkov I.V. Average background values of trace elements in minerals as criteria of geochemical specialization of precumbrian granitoids in Belarus. It has been established, that geochemical specialization of regional granitoids is largely dependent on the microelement composition of rock-forming minerals. Astapenko V.N., Aksamentova N.V. Structure of electrical conductivity in Belarus anteclise basement along Eurobridge geotransect.
Good correlation is shown between two types of sections.
Zones of high-temperature blastomylonites coincide with crustal anomalies of the electrical conductivity. Geological and pollen investigations revealed that these sediments were forming at the end of the Berezina Glaciation, then during the Alexandrian Interglacial and at the beginning of the Dnieper Glaciation. Lake and bog sediments are buried under the one till. The section Dobraya appears to be the most complete Middle Pleistocene section in eastern Belarus and may be recommended as the regional stratotype. Unlike the regional tensile stress field in the Pripyat paleorift, it is representative of the horizontal compression.