Zobrazeno 1 - 10
of 16
pro vyhledávání: '"N. N. Titkov"'
Autor:
N. V. Shestakov, G. V. Nechaev, N. N. Titkov, D. V. Chebrov, V. V. Pupatenko, А. S. Prytkov, K. A. Nagorny
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 3 (2024)
The mechanisms of preparation and occurrence of the strongest deep-focus earthquakes with MW≥8, as well as their surface manifestations, remain insufficiently studied because of the lack of the relevant data. There are but three seismic events of t
Externí odkaz:
https://doaj.org/article/8f91d1d954b8448e803c1147543f0636
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 6 (2023)
The paper presents the results of comparative analysis of the data regarding the multi-instrumental borehole monitoring data of changes in the geoenvironment stress-strain state and GPS data obtained in the time vicinity of the close strong Zhupanovs
Externí odkaz:
https://doaj.org/article/4a0e8bdb04d549f89c929eaa15bfb267
Autor:
S. Ya. Droznina, A. V. Lander, Yu.K. Serafimova, V. A. Saltykov, V. M. Pavlov, D. V. Chebrov, S. V. Mityushkina, N. N. Titkov, Yu.A. Kopytenko, I. R. Abubakirov
Publikováno v:
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 45, Iss 1, Pp 100-117 (2020)
The paper presents the first results of integrated research of the strong seismic event (Uglovoye Podnyatiye earthquake (UPE) with a magnitude of Mw=7.3) that occurred on December 20, 2018 in the junction zone between the Kuril-Kamchatka and Aleutian
Autor:
S. S. Serovetnikov, Hiroaki Takahashi, V. E. Glukhov, N. A. Zharinov, E. O. Makarov, P. P. Firstov, N. N. Titkov
Publikováno v:
Доклады Академии наук. 489:303-306
The set of parameters of geophysical fields and geodynamic events before the strongest Okhotsk Sea earthquake May 24, 2013 with MW = 8,3 and a focal depth of 630 km in this paper analyzed. In the temporary vicinity of the earthquake (May 19-20), ther
Autor:
N. A. Zharinov, E. O. Makarov, N. N. Titkov, Hiroaki Takahashi, V. E. Glukhov, P. P. Firstov, S. S. Serovetnikov
Publikováno v:
Doklady Earth Sciences. 489:1372-1375
This study analyzes the set of parameters of geophysical fields and geodynamic events before the very strong Sea of Okhotsk earthquake of May 24, 2013, with Mw = 8.3 and a focal depth of 630 km. In the time neighborhood of the earthquake (May 19–20
Autor:
S. Ya. Droznina, D. A. Ototyuk, D. V. Chebrov, N. N. Titkov, A. V. Lander, I. R. Abubakirov, A. A. Gusev, S. V. Mityushkina, Yu. A. Kugaenko, V. M. Pavlov
Publikováno v:
Izvestiya, Physics of the Solid Earth. 55:576-599
The largest instrumentally recorded regional back-arc earthquake with MW = 7.8, MC = 8.2 occurred on July 17, 2017 on the Bering transform fault (the boundary between the Beringia minor lithospheric plate and the Komandorskii (Commander) block of the
Autor:
M. Guojie, N. N. Titkov, M.D. Gerasimenko, Nikolay V. Shestakov, Hiroaki Takahashi, A.K. Kishkina, A.L. Verkhoturov, N.A. Gagarskii, D.V. Sysoev
Publikováno v:
Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa. 16:33-44
Autor:
N. F. Vasilenko, M. G. Kogan, D. I. Frolov, Grigory M. Steblov, Jeffrey T. Freymueller, N. N. Titkov, Göran Ekström, A. S. Prytkov
Publikováno v:
Geophysical Research Letters. 44:3176-3183
The Aleutian and Kuril-Kamchatka arcs meet at a triple junction of the Pacific (PAC), Bering (BER), and North American (NAM) plates. We invert GPS observations from the westernmost Aleutian (Komandorsky) Islands and Kamchatka for the fault locking de
Publikováno v:
Journal of Volcanology and Seismology. 9:258-275
—This paper is concerned with ground deformation and seismicity prior to the Tolbachik Fissure Eruption, which began in Kamchatka on November 27, 2012. Seismic and GPS data were analyzed to reveal synchronous precursory anomalies in crustal deforma
Publikováno v:
Journal of Volcanology and Seismology. 9:242-257
The seismic moment tensor (SMT) was computed for the source of the deep-focus Sea of Okhotsk earthquake of May 24, 2013 (M w = 8.3) based on two kinds of regional data: (1) coseismic displacements at GNNS stations; and (2) three-component broadband s