Instrumental recording of slow deformation waves in the South Baikal geodynamic study site
- Authors: Bornyakov S.A.1, Salko D.V.2, Seminsky K.Z.2, Demberel S.3, Ganzorig D.3, Batsaihan T.3, Togtohbayar S.3
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Affiliations:
- Irkutsk State University
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Issue: Vol 473, No 1 (2017)
- Pages: 371-374
- Section: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189558
- DOI: https://doi.org/10.1134/S1028334X17030229
- ID: 189558
Cite item
Abstract
Instrumental monitoring of rock deformation in the South Baikal geodynamic study site showed that they are realized in the form of long-term variations in different directions superimposed with short-time anomalous spikes. Analysis of the measured spatiotemporal monitoring series showed that anomalous deformations are caused by the propagation of deformation waves through the mountainous rocks. We estimated their lengths, periods, directions, and velocity of spatial migration. We found that propagation of deformation waves is accompanied by an increase in the temperature of rocks at each point of monitoring.
About the authors
S. A. Bornyakov
Irkutsk State University
Author for correspondence.
Email: bornyak@crust.irk.ru
Russian Federation, Irkutsk
D. V. Salko
Institute of the Earth’s Crust, Siberian Branch
Email: bornyak@crust.irk.ru
Russian Federation, Irkutsk, 664033
K. Zh. Seminsky
Institute of the Earth’s Crust, Siberian Branch
Email: bornyak@crust.irk.ru
Russian Federation, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Mongolia, Ulaanbaatar
D. Ganzorig
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Mongolia, Ulaanbaatar
T. Batsaihan
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Mongolia, Ulaanbaatar
S. Togtohbayar
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Mongolia, Ulaanbaatar
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