The effect of seismic density irregularities on the stress-strain state of the Earth's crust and mantle tops along the profile 1-SB
https://doi.org/10.18303/2619-1563-2025-4-30
Abstract
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.
About the Authors
R. A. BakeevRussian Federation
Koptyug Ave., 3, Novosibirsk, 630090
Yu. P. Stefanov
Russian Federation
Koptyug Ave., 3, Novosibirsk, 630090
E. A. Melnik
Russian Federation
Koptyug Ave., 3, Novosibirsk, 630090
V. D. Suvorov
Russian Federation
Koptyug Ave., 3, Novosibirsk, 630090
E. V. Pavlov
Russian Federation
Koptyug Ave., 3, Novosibirsk, 630090
A. S. Salnikov
Russian Federation
Koptyug Ave., 3, Novosibirsk, 630090
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Review
For citations:
Bakeev R.A., Stefanov Yu.P., Melnik E.A., Suvorov V.D., Pavlov E.V., Salnikov A.S. The effect of seismic density irregularities on the stress-strain state of the Earth's crust and mantle tops along the profile 1-SB. Russian Journal of Geophysical Technologies. 2025;(4):30-41. (In Russ.) https://doi.org/10.18303/2619-1563-2025-4-30
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