Beltir Earthquake, February 15, 2025 (Ms = 5.7, Altai Mountains): Results of Geological and Seismological Research in the Nearby Zone

An epicenter expedition was organized to the Altai Mountains by the Institute of Physics of the Earth RAS, to study the consequences of and conditions for the Beltir earthquake. The tremors in populated areas reached 6–7 in intensity. Overall there was minor damage to buildings, furniture, and other household items; some people experienced fright and poor health. There were secondary effects in the epicentral zone. They formed a compact area covering different geological and geomorphological conditions. The intensity in the epicentral area was 7. The seismic source is a locally activated structure manifested on the surface by an arch-shaped anticlinal fold measuring approximately 2.6 × 4.5 km.

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Publication Details

Journal
Doklady Earth Sciences
Published
2025-09-05
DOI
https://doi.org/10.1134/s1028334x25607862
Primary Topic
earthquake and tectonic studies
Type
article
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article

Beltir Earthquake, February 15, 2025 (Ms = 5.7, Altai Mountains): Results of Geological and Seismological Research in the Nearby Zone

Y. V. Butanayev, R. N. Vakarchuk, А.Н. Овсюченко, R. E. Tatevosyan et al.
Doklady Earth Sciences
earthquake and tectonic studies
article

Beltir Earthquake, February 15, 2025 (Ms = 5.7, Altai Mountains): Results of Geological and Seismological Research in the Nearby Zone

Y. V. Butanayev, R. N. Vakarchuk, А.Н. Овсюченко, R. E. Tatevosyan, N. G. Koshevoy, I. V. Matveev, S. A. Tikhotsky, A. S. Larkov, O. Yu. Kashitsyna, I. E. Parini
article en

Abstract

An epicenter expedition was organized to the Altai Mountains by the Institute of Physics of the Earth RAS, to study the consequences of and conditions for the Beltir earthquake. The tremors in populated areas reached 6–7 in intensity. Overall there was minor damage to buildings, furniture, and other household items; some people experienced fright and poor health. There were secondary effects in the epicentral zone. They formed a compact area covering different geological and geomorphological conditions. The intensity in the epicentral area was 7. The seismic source is a locally activated structure manifested on the surface by an arch-shaped anticlinal fold measuring approximately 2.6 × 4.5 km.

Doklady Earth SciencesVol. 524(2)
Siberian Branch of the Russian Academy of Sciences (RU), Schmidt Institute of Physics of the Earth (RU)
Openalex Percentile: Top 75%
earthquake and tectonic studies
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