Diagnostics of the stress state of the lithosphere in Mongolia based on seismic source data
- Autores: Klyuchevskii A.V.1, Demberel S.2, Dem’yanovich V.M.1, Bayaraa G.2
-
Afiliações:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Edição: Volume 473, Nº 2 (2017)
- Páginas: 433-437
- Seção: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189665
- DOI: https://doi.org/10.1134/S1028334X17040018
- ID: 189665
Citar
Resumo
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.
Sobre autores
A. Klyuchevskii
Institute of the Earth’s Crust, Siberian Branch
Autor responsável pela correspondência
Email: akluchev@crust.irk.ru
Rússia, ul. Lermontova 128, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Mongólia, Ulaanbaatar
V. Dem’yanovich
Institute of the Earth’s Crust, Siberian Branch
Email: akluchev@crust.irk.ru
Rússia, ul. Lermontova 128, Irkutsk, 664033
G. Bayaraa
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Mongólia, Ulaanbaatar
Arquivos suplementares
