Zobrazeno 1 - 10
of 22
pro vyhledávání: '"O. D. Zotov"'
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:
Journal of Volcanology and Seismology. 16:143-149
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6d84fef91d2d0c752e3aab09d0cde31
https://doi.org/10.1134/s0742046322020026
https://doi.org/10.1134/s0742046322020026
Publikováno v:
Journal of Volcanology and Seismology. 15:373-378
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::287e1702a060f2c9d49ab4d0bcab8b27
https://doi.org/10.1134/s0742046321060038
https://doi.org/10.1134/s0742046321060038
Autor:
Anatol Guglielmi, O. D. Zotov
Publikováno v:
Izvestiya, Physics of the Solid Earth. 57:567-572
—In their paper published in Izvestiya, Physics of the Solid Earth, G.A. Sobolev et al. (2020) discussed the results of their study. Firstly, it is noted that the most important element of the magnetic storm affecting seismicity is the Pc5 geomagne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e0692a430169650f09bf519ed7e15fc
https://doi.org/10.1134/s1069351321040054
https://doi.org/10.1134/s1069351321040054
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c55c542fa910085cf64850792ab08e80
https://doi.org/10.1134/s0742046321010139
https://doi.org/10.1134/s0742046321010139
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2f61bb78c7bf458b76724cbc953c77c
https://doi.org/10.1134/s0742046320050073
https://doi.org/10.1134/s0742046320050073
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9794cba397efb9e3b0400f0973c7a6e5
https://doi.org/10.31857/s0203-03062019679-84
https://doi.org/10.31857/s0203-03062019679-84
Publikováno v:
Journal of Volcanology and Seismology. 13:415-419
The Omori law for repeated underground shocks after a large earthquake is written here in the form of a nonlinear differential equation. We define a coefficient of deactivation for the rupture zone after the main shock. Two advantages of the new form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aeaaa20410428a481a5f37586742158c
https://doi.org/10.1134/s0742046319060034
https://doi.org/10.1134/s0742046319060034
Publikováno v:
Izvestiya, Physics of the Solid Earth. 54:178-191
Based on the observation data for hundreds of the main shocks and thousands of aftershocks, the existence of effect of round-the-world surface seismic waves is demonstrated (let us conditionally refer to them as a round-the-world seismic echo) and th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b2b858573ac5eb92d8d036344f0f053
https://doi.org/10.1134/s1069351318010159
https://doi.org/10.1134/s1069351318010159
Publikováno v:
Izvestiya, Physics of the Solid Earth. 53:10-17
Previously, we predicted and then observed in practice the property of aftershocks which consists in the statistically regular clustering of events in time during the first hours after the main shock. The characteristic quasi-period of clustering is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f99112570a84c3799befb70251ebbd09
https://doi.org/10.1134/s1069351317010086
https://doi.org/10.1134/s1069351317010086