Fault tectonics of the Ukhta fold in the Timan Ridge

he article deals with a model of the fault tectonics of the Ukhta fold in the Timan Ridge, created on the basis of reinterpretation of seismic data. By the results of constructions along the top of the Upper Proterozoic basement, the majority of the faults have a northwestern direction and extend both continuously and fragmentarily throughout the entire structure. Only north-west-directed faults are clearly traced over the surface of the Devonian deposits. The overlay of the obtained scheme onto the map of the anomalous magnetic field indicates that the identified faults are normally missed in the magnetic field when surveying at a scale of 1:50 000. For the detail site location of the faults and the continuous research of the geodynamic situation, a complex of field geophysical works is required to be conducted in the future.