SEISMICITY of the NORTH-EAST of RUSSIA in 2018–2019

Author:

Alyeshina E.I.1,Kurtkin S.V.1,Karpenko L.I.1

Affiliation:

1. Magadan branch of Geophysical Survey of the Russian Academy of Sciences

Abstract

The results of seismic monitoring of the Magadan region, Chukotka Autonomous Area and the shelf of adjacent Okhotsk, Chukchi, Bering and East Siberian seas are considered. There were 14 seismic stations working in the region. The catalog includes information about 644 earthquakes with energy classes KR=4.8–13.2. As usual, most of them (77 %) are localized in the Kolyma region (area № 2).The additional catalog contains information about 12 earthquakes in the Chukchi. The total seismic energy released within the region’s borders was ΣЕ=2.671013 J. The classification of Russian North-East earthquakes was performed using energy classes KR of T.G. Rautian’s scale. According to the earthquake energy representativeness map, the regional network of stations records without omissions the earthquakes with Kmin=7on the territory of Magadan region, with Kmin=8 in the Okhotsk sea and with Kmin=10 in the Chukchi. The strongest earthquake of 2018–2019 with KR=13.2 (MPSP=5.1, MS=4.0) occurred on July 5, 2019 in in the Kolyma area. 14 earthquakes with intensity I=2–5 of the Russian Seismic Intensity Scale (SIS-2017) were felt in North East settlements. Epicenters of Magadan region earthquakes were plotted on the tectonic zoning scheme. Most earthquakes are confined to the largest deep faults in the northwestern and sublatitudinal directions. All hypocenters are located within the earth's crust. The seismicity level of the North-East of Russia in 2018–2019 according to the “SOUS’09” scale was assessed as "background average one" for the observation period from 1968 to 2019. Spatially, all earthquakes in the North-East of Russia are traditionally concentrated in large seismogenic belts: Chersky, North-Okhotsk and Trans-Beringian.

Publisher

Geophysical Survey of the Russian Academy of Sciences - GS RAS

Subject

Aerospace Engineering

Reference24 articles.

1. Alyeshina, E.I., & Kurtkin, S.V. (2023). [Seismic stations North-East of Russia in 2018–2019 (network code NEGRS)]. Zemletriaseniia Severnoi Evrazii [Earthquakes in Northern Eurasia], 26(2018–2019). Electronic supplement. Retrieved from http://www.gsras.ru/zse/app-26.html (In Russ.).

2. Rautian, T.G. (1964). [On determining the energy of earthquakes at a distance of 3000 km]. In Eksperimental'naia seismika. Trudy IFZ AN SSSR № 32(199) [Experimental seismic] (pp. 88–93). Moscow, Russia: Nauka Publ. (In Russ.).

3. Artamonov, V.V., & Mishina, L.V. (1984). [Registration capabilities of the network of seismic stations of the North-East of the USSR]. In Seysmicheskie processy na Severo-Vostoke SSSR [Seismic processes in the North-East of the USSR] (pp. 99–115). Magadan, Russia. (In Russ.).

4. Droznin, D.V., & Droznina, S.Ya. (2011). Interactive DIMAS software for seismic signal processing. Seismic Instruments, 47(3), 215–224. DOI: https://doi.org/10.3103/S0747923911030054

5. Mackey, K.G. (1999). Seismological Studies in Northeast Russia. Dissertation for the degree of Ph.D. Michigan State University. Department of Geological Sciences, 346 р.

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