Zobrazeno 1 - 10
of 47
pro vyhledávání: '"A. D. Zavyalov"'
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 3 (2023)
The physics of earthquakes was contriubuted to by the concept of proper time of the source of a strong earthquake, which is different from universal (calendar) time. The earlier idea of proper time was implicit and has been considered only in relatio
Externí odkaz:
https://doaj.org/article/47120f4df9af4d61b1b6f5b383866f33
Publikováno v:
Геодинамика и тектонофизика, Vol 5, Iss 1, Pp 321-326 (2015)
The 9th International Workshop “Physics and Forecasting of Rock Destruction” was held in the Institute of the Earth’s Crust, SB RAS, in Irkutsk on 02–06 September 2013. The article reviews the main events of this scientific forum and briefly
Externí odkaz:
https://doaj.org/article/5c186651d2b14440aa9d4969754a051f
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 58:908-924
Publikováno v:
Journal of Volcanology and Seismology. 16:143-149
Autor:
V. A. Pavlenko, A. D. Zavyalov
Publikováno v:
Izvestiya, Physics of the Solid Earth. 58:89-105
—The magnitude of completeness $${{M}_{c}}$$ of the earthquakes above which 100% of events are thought to be reliably detected is a vital parameter characterizing the completeness of seismic data. A known fact is that to obtain correct estimates of
Publikováno v:
Journal of Volcanology and Seismology. 15:373-378
Publikováno v:
Doklady Earth Sciences. 496:80-85
The time dependences of the fracture concentration parameter characterizing the process of accumulation of defects formed in loaded objects, i.e., steel specimens in laboratory experiments and in the source zone of a strong earthquake, are obtained.
Autor:
O. D. Zotov, A. D. Zavyalov
Publikováno v:
Journal of Volcanology and Seismology. 15:19-25
This paper presents the results of analysis of the spatial distribution of repeated shocks. Data from the world earthquake catalog of USGS/NEIC from 1973 to 2014 were used. Short time intervals, no more than 10 hours after the main shock, and distanc
Publikováno v:
Journal of Volcanology and Seismology. 14:341-352
In recent years three new problems emerged in aftershock physics. We shall refer to these problems in a preliminary way as the dynamic, the inverse, and the morphological problem. They have been distinctly stated, partially solved, and have a fundame
Publikováno v:
Вулканология и сейсмология. :79-84
The Omori Law, which describes the repeated underground shocks after a strong earthquake, is written in the form of a nonlinear differential equation. An idea of the focal deactivation coefficient after the main shock is introduced. Two advantages of