Instrumental recording of slow deformation waves in the South Baikal geodynamic study site
- Авторлар: 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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Мекемелер:
- Irkutsk State University
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Шығарылым: Том 473, № 1 (2017)
- Беттер: 371-374
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189558
- DOI: https://doi.org/10.1134/S1028334X17030229
- ID: 189558
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
S. Bornyakov
Irkutsk State University
Хат алмасуға жауапты Автор.
Email: bornyak@crust.irk.ru
Ресей, Irkutsk
D. Salko
Institute of the Earth’s Crust, Siberian Branch
Email: bornyak@crust.irk.ru
Ресей, Irkutsk, 664033
K. Seminsky
Institute of the Earth’s Crust, Siberian Branch
Email: bornyak@crust.irk.ru
Ресей, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Моңғолия, Ulaanbaatar
D. Ganzorig
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Моңғолия, Ulaanbaatar
T. Batsaihan
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Моңғолия, Ulaanbaatar
S. Togtohbayar
Institute of Astronomy and Geophysics
Email: bornyak@crust.irk.ru
Моңғолия, Ulaanbaatar
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