Deep structure model of Pechora-Barents Sea Basin based on interpretation of gravimetric data
A modern deep structure model of Pechora-Barents Sea region is constructed on the basis of complex geological and geophysical studies. The increase in reliability of the results is achieved by using the technique of structural and dense geological modeling. The researches performed make it possible to construct the schemes of the main boundaries of the earth’s crust separation (Moho-Conrad discontinuity), to study thickness of the layers under study and establish density non-uniformities within their boundaries.