STATISTICAL ESTIMATIONS OF THE RELATIONSHIP OF REGIONAL MAGNETIC ANOMALIES WITH SEISMIC BORDERS OF THE URALS REGION NETHER-POLAR SECTOR
For nether-polar Eurasian sector within the coordinates 60–68° N, 48–72° E statistical studies have shown that the regional magnetic anomalies can’t be explained by changes in the basement topography and the Moho, as well as variations in the thickness of the consolidated crust and basalt layer. The correlation coefficient between the intensity of regional magnetic anomalies and variations in the crust boundaries relief reaches the maximum value for the surface of basalt layer. The conclusions, in the study area, the lower limit of the magnetically active layer of the lithosphere is located significantly higher Moho and the main contribution to regional magnetic anomalies introduced the top surface of the basalt layer.