DEFORMATION ANOMALIES OF THE TSUNAMIGENIC EARTHQUAKE OF JULY 29, 2025

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Abstract

The article describes the deformation anomalies recorded by remote laser strainmeters, and provides estimates of the displacement of the seabed in the focus of the tsunamigenic earthquake that led to the tsunami.

About the authors

G. I Dolgikh

V.I. Ilyichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Email: dolgikh@poi.dvo.ru
Academician of the RAS Vladivostok, Russia

Yu. N Kulchin

Institute of Automation and Control Processes, Far Eastern Branch of the Russian Academy of Sciences

Academician of the RAS Vladivostok, Russia

S. G Dolgikh

V.I. Ilyichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences; Institute of Automation and Control Processes, Far Eastern Branch of the Russian Academy of Sciences

Corresponding Member of the RAS Vladivostok, Russia; Vladivostok, Russia

A. V Myasnikov

P.K. Shternberg State Astronomical Institute, Lomonosov Moscow State University

Moscow, Russia

References

  1. Gusiakov V.K. Relationship of tsunami intensity to source earthquake magnitude as retrieved from historical data // Pure Appl. Geophys. 2011. 16820332041.
  2. Titov V.V., Song Y.T., Tang L. et al. Consistent estimates of tsunami energy show promise for improved early warning // Pure and Applied Geophysics. 2016. No. 173(12). P. 3863–3880. https://doi.org/10.1007/s00024-016-1312-1 https://earthquake.usgs.gov/earthquakes/
  3. Долгих Г.И., Долгих С.Г., Ковалёв С.Н., Корень И.А., Овчаренко В.В., Чупин В.А., Швец В.А., Яковенко С.В. Регистрация деформационной аномалии цунамигенного землетрясения лазерным деформографом // ДАН. 2007. Т. 412. № 1. С. 104‒106.
  4. Dolgikh G., Dolgikh S. Deformation Anomalies Accompanying Tsunami Origination // J. Mar. Sci. Eng. 2021. V. 9. P. 1144.
  5. Dolgikh G., Dolgikh S. Deformation Anomalies Accompanying Tsunami Origins near the Japanese Islands // J. Mar. Sci. Eng. 2023. V. 11. P. 2137. https://doi.org/10.3390/jmse11112137

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