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Autor:
A. A. Dobrynina, Vladimir Chechelnitsky, Vladimir San'kov, Munkhuu Ulzibat, Victor I. German, Larisa R. Tcydypova
Publikováno v:
Journal of Seismology. 24:1297-1305
We again give thanks to A. Sorokin and A. Klyuchevskii and the Editorial Board of the Journal for the opportunity to discuss our results that have been published in the “Journal of Seismology” (Dobrynina, A.A., Sankov, V.A., Tcydypova, L.R., Germ
Autor:
Dobrynina, Anna A., Sankov, Vladimir A., Tcydypova, Larisa R., German, Victor I., Chechelnitsky, Vladimir V., Ulzibat, Munkhuu
Publikováno v:
Journal of Seismology; 2020, Vol. 24 Issue 6, p1297-1305, 9p
Publikováno v:
Geoscience Frontiers, Vol 8, Iss 6, Pp 1323-1337 (2017)
Lithospheric stress in Mongolia has been studied using mechanisms of 84 MLH ≥ 4 earthquakes that occurred in the 20th century and instrumental seismic moments of 17,375 MLH ≥ 2.5 events recorded between 1970 and 2000. The MLH ≥ 3.5 earthquakes
Autor:
Anatoly V. Klyuchevskii
Publikováno v:
Journal of Asian Earth Sciences. 88:246-256
The current geodynamics and tectonophysics of the Baikal rift system (BRS) as recorded in lithospheric stress and strain are discussed in the context of self organization of nonlinear dissipative dynamic systems and nonlinear media. The regional stra
Autor:
Anatoly V. Klyuchevskii
Publikováno v:
Journal of Geodynamics. 49:19-23
This is an attempt to analyze the current lithospheric stress pattern in the Baikal rift in terms of nonlinear dynamics as an open self-organizing system in order to gain more insights into the general laws of regional seismicity. According to the su
Autor:
Anatoly V. Klyuchevskii
Publikováno v:
Journal of Geodynamics. 37:155-168
The investigation of spatio-temporal variations of seismic moments of earthquakes in the Baikal region shows three considerable episodes of change of the state of stress and strain of the Earth's crust between 1968 and 1994. The changes in the state
Publikováno v:
Geoscience Frontiers, Vol 4, Iss 6, Pp 709-716 (2013)
The current lithospheric geodynamics and tectonophysics in the Baikal rift are discussed in terms of a nonlinear oscillator with dissipation. The nonlinear oscillator model is applicable to the area because stress change shows up as quasi-periodic in
Publikováno v:
Journal of Seismology; 2020, Vol. 24 Issue 6, p1291-1296, 6p