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VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION

Year 2025, Volume: 27 Issue: 1, 10 - 14, 30.05.2025

Abstract

The article studies data on anomalous changes in the geomagnetic field stress near the earthquake source. The nature of the seismomagnetic effect is determined by the geomagnetic
regime in the source. The spatio-temporal distribution of the geomagnetic field stress gradient reflects the geodynamic regime in the Middle Kura depression.

References

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  • 2. Rzayev A.Q., Yetirmishli G.J., Kazimova S.E. 2013.Baku. Reflection of the geodynamic regime in variations of geomagnetic field strength. News. Geosciences, №4 pp. 3-5. (original in Azerbaijan)
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  • 6. Rzayev A.G. Identification of potential zones of seismotectonic deformations based on magnetometric data Catalogue of RSSC ANAS seismological observations on the territory of Azerbaijan in 2010, Baku 2014 (original in Russian)
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There are 9 citations in total.

Details

Primary Language English
Subjects Seismology and Seismic Exploration, Geophysics (Other)
Journal Section Research Article
Authors

Azay Rzayev This is me

Mahira Mammadova This is me

Publication Date May 30, 2025
Submission Date February 10, 2025
Acceptance Date April 15, 2025
Published in Issue Year 2025 Volume: 27 Issue: 1

Cite

APA Rzayev, A., & Mammadova, M. (2025). VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION. Seismoprognosis Observations in the Territory of Azerbaijan, 27(1), 10-14. https://doi.org/10.59849/2219-6641.2025.1.10
AMA Rzayev A, Mammadova M. VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION. Seismoprognosis Observations in the Territory of Azerbaijan. May 2025;27(1):10-14. doi:10.59849/2219-6641.2025.1.10
Chicago Rzayev, Azay, and Mahira Mammadova. “VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION”. Seismoprognosis Observations in the Territory of Azerbaijan 27, no. 1 (May 2025): 10-14. https://doi.org/10.59849/2219-6641.2025.1.10.
EndNote Rzayev A, Mammadova M (May 1, 2025) VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION. Seismoprognosis Observations in the Territory of Azerbaijan 27 1 10–14.
IEEE A. Rzayev and M. Mammadova, “VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION”, Seismoprognosis Observations in the Territory of Azerbaijan, vol. 27, no. 1, pp. 10–14, 2025, doi: 10.59849/2219-6641.2025.1.10.
ISNAD Rzayev, Azay - Mammadova, Mahira. “VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION”. Seismoprognosis Observations in the Territory of Azerbaijan 27/1 (May2025), 10-14. https://doi.org/10.59849/2219-6641.2025.1.10.
JAMA Rzayev A, Mammadova M. VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION. Seismoprognosis Observations in the Territory of Azerbaijan. 2025;27:10–14.
MLA Rzayev, Azay and Mahira Mammadova. “VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION”. Seismoprognosis Observations in the Territory of Azerbaijan, vol. 27, no. 1, 2025, pp. 10-14, doi:10.59849/2219-6641.2025.1.10.
Vancouver Rzayev A, Mammadova M. VARIATIONAL CHARACTERISTICS OF THE SEISMOMAGNETIC EFFECT (SME) DURING THE SAATLY-SABIRABAD BOUNDARY EARTHQUAKE THAT OCCURRED IN THE MIDDLE KURA DEPRESSION. Seismoprognosis Observations in the Territory of Azerbaijan. 2025;27(1):10-4.