Diagnostics of the stress state of the lithosphere in Mongolia based on seismic source data
- Авторы: Klyuchevskii A.V.1, Demberel S.2, Dem’yanovich V.M.1, Bayaraa G.2
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Учреждения:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Выпуск: Том 473, № 2 (2017)
- Страницы: 433-437
- Раздел: Geophysics
- URL: https://bakhtiniada.ru/1028-334X/article/view/189665
- DOI: https://doi.org/10.1134/S1028334X17040018
- ID: 189665
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Аннотация
The obtained results indicate that earthquakes of Mongolia form under the conditions of an alternating field of regional stresses, which is related to pulsed activations in the BRS and superimposed on the quasi-stationary field of global stresses of the Earth.
Об авторах
A. Klyuchevskii
Institute of the Earth’s Crust, Siberian Branch
Автор, ответственный за переписку.
Email: akluchev@crust.irk.ru
Россия, ul. Lermontova 128, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Монголия, Ulaanbaatar
V. Dem’yanovich
Institute of the Earth’s Crust, Siberian Branch
Email: akluchev@crust.irk.ru
Россия, ul. Lermontova 128, Irkutsk, 664033
G. Bayaraa
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Монголия, Ulaanbaatar
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