Construction of regional geophysical models based on the joint interpretation of gravitaty and seismic data

The technique of solving the inverse structural gravity problem based on the joint interpretation of gravity and seismic data is described in this paper. The method of solving is based on the method of local corrections, but involves some modifications described in the paper. An area of the northeastern part of the Urals and West Siberia (60°-65°N, 54°-72°E) was studied with the use of this technology and the spatial position of the boundaries of the crystalline crust of the Earth (its roof K₀ and base M) were determined from seismic and gravity data.     

Velocity and Density Cross Sections of the Upper Part of the Lithosphere within the North Urals Segment

Izvestiya, Physics of the Solid Earth - Abstract—The seismic data acquired by the Bazhenov Geophysical Expedition on the regional DSS profiles are revised to study the structure of the...     

Conjugacy Problem for Stationary Heat Fields

Doklady Earth Sciences - An analytical solution for the stationary problem of thermal conjugation is obtained for the model of inhomogeneous layered media. The heat flux components for the crust...