مجله ژئوفیزیک ایران

مجله ژئوفیزیک ایران

Investigation of temporal changes of seismicity and magnetic parameters before earthquakes with a magnitude of around 6 in Iran in 2017

نوع مقاله : مقاله پژوهشی‌

نویسندگان
1 M.Sc., Institute of Geophysics, University of Tehran, Tehran, Iran
2 Associate Professor, Institute of Geophysics, University of Tehran, Tehran, Iran
3 Associate Professor, Institute of Geophysics, University of Tehran, Tehran, Iran Associate Professor, Department of physics education, Farhangian University, Tehran, Iran
10.30499/ijg.2026.435424.1567
چکیده
This study examines temporal changes in seismicity and solar-geomagnetic parameters prior to moderate-to-large earthquakes in Iran during 2017-2018, with emphasis on the evolution of the Gutenberg-Richter b-value as a potential indicator of changing seismic regime. We selected five significant earthquakes for detailed analysis. While the study primarily focuses on main shocks with magnitudes around 6, the 2017 M 5.2 Malard (Tehran) earthquake was specifically included due to its proximity to the capital, affecting a population of over 10 million, and its status as the most significant instrumental event near Tehran in recent decades. Declustered earthquake catalogs from the Iranian Seismological Center (IRSC) were used to track b-value variations, while external parameters - including Earth’s magnetic field strength, solar wind proton density, geomagnetic indices including Disturbance Storm Time (Dst) and planetary K index (Kp), sunspot number, and 10.7 cm solar radio flux (F10.7 index) concerning fluctuations in b-value preceding major earthquakes - were analyzed at daily, hourly and 27‑day resolutions. In four out of five cases, the b-value showed a pronounced decrease within several weeks before the mainshock, indicating a temporary shift toward the dominance of larger-magnitude events, consistent with stress concentration patterns observed in prior studies. Four mainshocks also occurred when sunspot numbers and the F10.7 index were near their minimum values over the study period, whereas 27‑day averaged proton density tended to be relatively high close to the occurrence times. Moreover, the Kp index displayed low 27‑day averages for four events, and Dst and Kp indices showed localized anomalies within ±48 hours of some mainshocks. These patterns suggest possible temporal associations between seismic and solar-geomagnetic variability at monthly timescales, although no formal statistical tests were applied. However, the small number of events, uncertainties in the seismic and magnetic datasets and the absence of formal statistical testing limit the strength of any conclusions and preclude causal inference. The correlations identified here should therefore be regarded as preliminary and do not imply that solar or geomagnetic activity directly triggers earthquakes; rather, they suggest that solar-magnetic parameters may offer complementary contextual information on the evolving state of the crust when used alongside conventional seismotectonic indicators, motivating further studies with larger datasets and more rigorous statistical and physical modeling frameworks.
کلیدواژه‌ها

موضوعات


عنوان مقاله English

Investigation of temporal changes of seismicity and magnetic parameters before earthquakes with a magnitude of around 6 in Iran in 2017

نویسندگان English

Pooyan Hasan Beygi 1
Ali Moradi 2
Mohammad Javad Kalaee 3
1 M.Sc., Institute of Geophysics, University of Tehran, Tehran, Iran
2 Associate Professor, Institute of Geophysics, University of Tehran, Tehran, Iran
3 Associate Professor, Institute of Geophysics, University of Tehran, Tehran, Iran Associate Professor, Department of physics education, Farhangian University, Tehran, Iran
چکیده English

This study examines temporal changes in seismicity and solar-geomagnetic parameters prior to moderate-to-large earthquakes in Iran during 2017-2018, with emphasis on the evolution of the Gutenberg-Richter b-value as a potential indicator of changing seismic regime. We selected five significant earthquakes for detailed analysis. While the study primarily focuses on main shocks with magnitudes around 6, the 2017 M 5.2 Malard (Tehran) earthquake was specifically included due to its proximity to the capital, affecting a population of over 10 million, and its status as the most significant instrumental event near Tehran in recent decades. Declustered earthquake catalogs from the Iranian Seismological Center (IRSC) were used to track b-value variations, while external parameters - including Earth’s magnetic field strength, solar wind proton density, geomagnetic indices including Disturbance Storm Time (Dst) and planetary K index (Kp), sunspot number, and 10.7 cm solar radio flux (F10.7 index) concerning fluctuations in b-value preceding major earthquakes - were analyzed at daily, hourly and 27‑day resolutions. In four out of five cases, the b-value showed a pronounced decrease within several weeks before the mainshock, indicating a temporary shift toward the dominance of larger-magnitude events, consistent with stress concentration patterns observed in prior studies. Four mainshocks also occurred when sunspot numbers and the F10.7 index were near their minimum values over the study period, whereas 27‑day averaged proton density tended to be relatively high close to the occurrence times. Moreover, the Kp index displayed low 27‑day averages for four events, and Dst and Kp indices showed localized anomalies within ±48 hours of some mainshocks. These patterns suggest possible temporal associations between seismic and solar-geomagnetic variability at monthly timescales, although no formal statistical tests were applied. However, the small number of events, uncertainties in the seismic and magnetic datasets and the absence of formal statistical testing limit the strength of any conclusions and preclude causal inference. The correlations identified here should therefore be regarded as preliminary and do not imply that solar or geomagnetic activity directly triggers earthquakes; rather, they suggest that solar-magnetic parameters may offer complementary contextual information on the evolving state of the crust when used alongside conventional seismotectonic indicators, motivating further studies with larger datasets and more rigorous statistical and physical modeling frameworks.

کلیدواژه‌ها English

Earthquake precursor
seismic b-value
magnetic storms
solar proton
solar activity
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