НЕОТЕКТОНИКА И НЕФТЕНОСНОСТЬ ГЕОСТРУКТУР ТАТАРСТАНА

Spatial-varied neotectonic movements within the Tatarstan territory results in the rearrangement of the structural pattern of crystalline basement, sediment cover and day surface. The straight correlation is observed between oil reserves of geostructures and their neotectonic regime: the upward movements cause the inflow of oil-fluids from their generative origin to positive structures. The downcast movements lead to squeezing fluids from the structure.