Author
Listed:
- A. L. Sobisevich
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- G. M. Steblov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- A. A. Sentsov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- E. V. Deev
(Russian Academy of Sciences
Novosibirsk State University)
- L. V. Eppelbaum
(Tel Aviv University
Azerbaijan State Oil and Industry University)
- A. O. Agibalov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences
Moscow State University)
- I. M. Aleshin
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- G. R. Balashov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- O. T. Kamenev
(Institute of Automation and Control Processes of the Far Eastern Branch of the Russian Academy of Sciences)
- A. N. Kotov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- V. M. Makeev
(Sergeev Institute of Environmental Geoscience RAS)
- V. P. Perederin
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- F. V. Perederin
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- N. K. Rosenberg
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- K. I. Kholodkov
(Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences)
- O. V. Safronov
(Russian Academy of Sciences
Novosibirsk State University)
Abstract
The usefulness of identifying seismically active zones in the Altai-Sayan region has been demonstrated through the analysis of anomalies in three morphometric terrain parameters (depth of vertical dissection, average height, and difference between second-order and third-order base level surfaces), processed using fuzzy logic tools. According to GNSS data and earthquake focal mechanisms, active faults strike-slip tectonic settings, where the major compression axis strikes northeast. Computer simulations have shown that this process leads to the accumulation of extensional horizontal stress in zones occupying approximately 50% of the investigated area, where 72% of all earthquake epicenters are localized and 83% of those have a moment magnitude of 5.5 or greater. The results of the morphometric terrain analysis and computer simulation enabled the delineation of 13 potential earthquake source zones with moment magnitudes Mw ≥ 5.5. Their configuration aligns well with observed recent seismicity trends and paleoseismological evidence.
Suggested Citation
A. L. Sobisevich & G. M. Steblov & A. A. Sentsov & E. V. Deev & L. V. Eppelbaum & A. O. Agibalov & I. M. Aleshin & G. R. Balashov & O. T. Kamenev & A. N. Kotov & V. M. Makeev & V. P. Perederin & F. V., 2025.
"Identification of potential earthquake source locations zones in the Altai-Sayan mountain region: a new approach based on the morphometric terrain analysis and the geodynamic modeling,"
Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 121(17), pages 19863-19887, October.
Handle:
RePEc:spr:nathaz:v:121:y:2025:i:17:d:10.1007_s11069-025-07596-3
DOI: 10.1007/s11069-025-07596-3
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