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The Regional Tidal Response of the Geophysical Medium

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An Erratum to this article was published on 01 May 2022

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Abstract

The results of long-term experimental observations of tidal deformations of the Earth’s crust are reported. These studies have been conducted with the use of the unique laser interferometer of the Sternberg State Astronomical Institute (GAISh), Moscow State University, installed in the deep underground tunnel of the Baksan Neutrino Observatory. A fifteen-year series of continuous in-situ observations of the lithospheric deformations and the corresponding theoretical calculated values of the tide with the basic lunar wave M2 being distinguishing have been analyzed. The features of the tidal response have been studied for a given volume of the layered geophysical medium on the basis of the data obtained. Changes in the amplitude and phase parameters of the medium were analyzed taking into consideration the patterns of the seismic process. The possibilities of using the parameters of the tidal response of the geophysical medium as possible indicators of the formation and development of focal structures of regional seismic events were considered.

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ACKNOWLEDGMENTS

The authors are grateful to the staff of the observatory, engineers N.A. Perelygin and S.V. Girin, for technical support of the Baksan laser interferometer.

Funding

This work was supported by the Russian Science Foundation, project no. 19-05-00341.

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Authors and Affiliations

  1. Sternberg State Institute of Astronomy, Moscow State University, 119234, Moscow, Russia

    A. V. Myasnikov

  2. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123995, Moscow, Russia

    L. E. Sobisevich & D. V. Likhodeev

Authors
  1. A. V. Myasnikov
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  2. L. E. Sobisevich
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  3. D. V. Likhodeev
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Corresponding author

Correspondence to A. V. Myasnikov.

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The authors declare that they have no conflicts of interest.

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Translated by V. Krutikova

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Myasnikov, A.V., Sobisevich, L.E. & Likhodeev, D.V. The Regional Tidal Response of the Geophysical Medium. Dokl. Earth Sc. 503, 205–210 (2022). https://doi.org/10.1134/S1028334X22040146

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  • DOI: https://doi.org/10.1134/S1028334X22040146

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