The effect of seismic density irregularities on the stress-strain state of the Earth's crust and mantle tops along the profile 1-SB

Using the results of seismic density modeling on the 1-SB profile, the stress-strain state arising under the influence of gravity forces in the Earth's crust of the Baikal folded region was numerically studied. It has been shown that the main role in the formation of inhomogeneities of the stressed state and its anomalies is played by variations in the thickness and depth of layers of rocks with different physical and mechanical properties.