At the end of the sixties, the Laboratory for Modeling of Geological Processes was established for the purpose of mathematical analysis of oil and gas information.

Dynamic conditions of formation of discontinuous systems in the sedimentary cover of the Siberian Platform in the area of the Kovykta gas condensate field, which existed in the Paleozoic and Cenozoic, are consistent with those for its southern margin, which allows us to speak about their possible relationship with the determining role of the latter in relation to the former. The Kovykta area is more than 100 km away from the southern margin of the Siberian Platform. In this connection the presence of the discussed relationship requires additional argumentation in the form of substantiation of physical possibility of deformation transmission through the sedimentary cover to such a distance from the platform edge.

The authors have performed physical modeling of the geodynamic conditions of NW compression, left-lateral shear, and SW extension, which operated on the southern margin of the Siberian Platform in the Paleozoic, Early Cenozoic, and Middle-Late Cenozoic, respectively, under similarity conditions. The modeling results showed that, under certain boundary conditions of the experiments, deformations can propagate from the edge of the model to its interior over long distances only under compression and tension. Under shear conditions, the lateral dimensions of the area of spatial propagation of deformations in the model are always smaller than those observed in its natural counterpart. This indicates that the Early Cenozoic dynamic environment of left shear in the sedimentary cover of the Kovykta gas condensate field area owes its origin to the complex of geodynamic processes on all active margins of the Siberian Platform.