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Information × Registration Number 0206U002405, 0103U001896 , R & D reports Title Structure and geodynamics of the Ukrainian shield and Voronezh massif joint zone in the Precambrian and Paleozoic stages popup.stage_title Head Sivoronov Albert Oleksijovych, Registration Date 07-02-2006 Organization Ivan Franko Lviv National University popup.description2 Ukrainian shield (USh) and Voronezh crystalline massif (VCM) are formed by the same types Early Precambrian complexes and belong to the same I-st rank structure - Voronezh-Ukrainian geoblock of the East-European platform. Nethertheless, they developed autonomically from the beginning of the Late Achaean (or maybe earlier). The geodynamic model is considered for the Late Achaean stage. It is supposed that the greenstone structures were formed during this stage in stress conditions which had different orientation in the USh and VCM. The North-West line, dividing USh and VCM in this time corresponded to the regional tectonic fault. The Donetzk-Dnieprian Trough (DDT) inherited this fault in Fanerozoic. This and other faults, emerged in Achaean time, made the strong influence on the DDT sediments structure and gas-oil saturation. Product Description popup.authors popup.nrat_date 2020-04-02 Close