Diagnostics of the stress state of the lithosphere in Mongolia based on seismic source data
- Авторлар: Klyuchevskii A.V.1, Demberel S.2, Dem’yanovich V.M.1, Bayaraa G.2
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Мекемелер:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Шығарылым: Том 473, № 2 (2017)
- Беттер: 433-437
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189665
- DOI: https://doi.org/10.1134/S1028334X17040018
- ID: 189665
Дәйексөз келтіру
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.
Авторлар туралы
A. Klyuchevskii
Institute of the Earth’s Crust, Siberian Branch
Хат алмасуға жауапты Автор.
Email: akluchev@crust.irk.ru
Ресей, ul. Lermontova 128, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Моңғолия, Ulaanbaatar
V. Dem’yanovich
Institute of the Earth’s Crust, Siberian Branch
Email: akluchev@crust.irk.ru
Ресей, ul. Lermontova 128, Irkutsk, 664033
G. Bayaraa
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Моңғолия, Ulaanbaatar
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