SPECTRAL and FOCAL PARAMETERS of NORTHERN CAUCASUS EARTHQUAKES in 2016–2017

Author:

Malyanova L.S.1,Zvereva A.S.1,Gabsatarova I.P.1

Affiliation:

1. Geophysical Survey of the Russian Academy of Sciences

Abstract

The source spectral and dynamic parameters for 39 earthquakes with KR=10.0–13.8 occurred in the North Caucasus for 2016–2017 are given. The parameters were determined from S-wave amplitude spectra. Records of four regional digital seismic stations («Anapa», «Kislovodsk», «Makhachkala» and «Sochi») located no more than 300 km from the sources were used. The values of the frequency-dependent quality factor Q(f) for the environment near these stations were obtained earlier. This is necessary to take into account the attenuation of S-wave energy in the Earth's crust and upper mantle in order to recalculate the station spectra into the source spectra. In 2016–2017, most of the studied earthquakes were located in the Eastern Caucasus. For the first time, for western zone earthquakes recorded by a network of stations (N=4–7), the SEISAN program was applied and satisfactory results were obtained when compared with the Crimean data for the Kerch-Kuban zone.

Publisher

Geophysical Survey of the Russian Academy of Sciences - GS RAS

Subject

Aerospace Engineering

Reference17 articles.

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2. Pavlenko, O.V. (2016). [Characteristics of the seismic waves attenuation in the Northern Caucasus estimated from records at seismic stations «Sochi» and «Anapa»]. Voprosy inzhenernoy seysmologii [Seismic Instru-ments], 43(1), 49–61. (In Russ.).

3. Pavlenko, O.V. (2009). The study of the radiation characteristics and propagation of seismic waves in the North Caucasus by modeling the accelerograms of the recorded earthquakes. Izvestiya, Physics of the Solid Earth, 45(10), 874–884.

4. Pavlenko, O.V. (2020). Seismic Wave Absorption in the Eastern Part of the North Caucasus Estimated from the Records of Seismic Station «Makhachkala». Izvestiya, Physics of the Solid Earth, 56(5), 635–643.

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