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:: Volume 12, Issue 3 (3-2023) ::
JGST 2023, 12(3): 39-50 Back to browse issues page
Monitoring of ground movement and estimation of earthquake fault parameters using Sentinel-1 data (Case study: Genaveh earthquake)
Ebrahim Karami , Niloofar Alizadeh , Mahmoodreza Sahebi *
Abstract:   (704 Views)
Given the special situation of Iran in terms of tectonics, it can be claimed that all faults in the country are seismic. Every year, financial and human losses and losses occur, especially in rural areas due to earthquakes. Today, interferometry synthetic aperture radar technology with various capabilities and products in the field of phase and amplitude has become a powerful tool for monitoring movements. Satellite imagery for two-pass (ascending and descending) capture can provide different information about faults. In this paper, seismic fault parameters are estimated by solving the inverse problem with surface displacement field boundary values ​​obtained from InSAR observations. The study of active fault parameters to identify earthquakes and improve their predictability is a topic of interest for geologists. For this purpose, a pair of Sentinel-1 radar images before and after the earthquake have been studied as images of the study area. As the results show, the maximum amount of ground displacement was 19 cm up and 8 cm down. To obtain the fault geometry and slip distribution on the fault plane, these components have been inverted using the genetic algorithm optimization method and the Acada ​​elastic half-space analysis model. The inverse modeling method showed that InSAR is a useful method for estimating the amount of ground displacement due to an earthquake and also determining the parameters of the fault causing the earthquake. Also, there is 1 and 3 cm uncertainty for two observed and modeled data, respectively. This indicates a better accuracy of descending geometry.
Article number: 3
Keywords: Keyword: earthquake, InSAR, modeling, ascending, descending, fault
Full-Text [PDF 1601 kb]   (311 Downloads)    
Type of Study: Research | Subject: Photo&RS
Received: 2022/02/15
References
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19. Howard A. Zebker, Richard M. Goldstein . 1986Topographic mapping from interferometric synthetic aperture radar observations [DOI:10.1029/JB091iB05p04993]
20. K. Gabriel, Richard M. Goldstein, Howard A. Zebker at 1989 Mapping small elevation changes over large areas: Differential radar interferometry Andrew. [DOI:10.1029/JB094iB07p09183]
21. Wright, T. J., Parsons, B. E. and Lu, Z., 2004, Toward mapping surface deformation in three dimensions using InSAR, Geophys. Res. Lett., 31,L01607, doi:10.1029/2003GL018827. [DOI:10.1029/2003GL018827]
22. Yasser Maghsoudi, Sahel Mahdavi, "Principle of Radar"
23. S Karimzadeh, M Matsuoka, M Miyajima, B Adriano, A Fallahi , J Karashi, " Sequential SAR Coherence Method for the Monitoring of Buildings in Sarpole-Zahab, Iran", Remote sensing and Envirment, 10, 1255,2018 [DOI:10.3390/rs10081255]
24. Berberian, M. (1995) Master Blind Thrust Faults Hidden under the Zagros Folds: Active Basement Tectonics and Surface Morphotectonics. Tectonophysics Journal, 241, 193-224. [DOI:10.1016/0040-1951(94)00185-C]
25. H Beran GUNCE, B Taner SAN, " Measuring Earthquake-Induced Deformation in the South of Halabjah (Sarpol-e-Zahab) Using sentinel-1 Data on November 12, 2017", Proceedings, 2, 346,2018. [DOI:10.3390/ecrs-2-05159]
26. C Tolomei, N Svigkas, A Fathian Baneh, S Atzori, G Pezzo, " Surface Deformation And Sourse Modeling For The MW 7.3 IRAN Earthquake (November 12, 2017) Exploiting sentinel-1 AND ALOS-2 INSAR Data ", IGARSS, Vol. 14, 3071-4, 2018. [DOI:10.1109/IGARSS.2018.8518173]
27. M Motage , S Vajedian, R Behling, M Haghshenas Haghighi, D scheffler, S Roessner, B Akbari, H Wetzel, and A Darabi, " 12 November 2017 Mw 7.3 Sarpol-e Zahab, Iran, earthquake: Results from combining radar and optical remote sensing measurements with geophysical modeling and field mapping ", EGU General Assembly, Vol. 20, EGU2018-10528-4, 2018.
28. Okada, Y. (1985). "Surface deformation due to shear and tensile faults in a half-space", Bulletin of the Seismological Society of America, 75(4), 1135-1154. [DOI:10.1785/BSSA0750041135]
29. Pakdaman , Z golshadi , et . (2017) . Effect parameters are optimized for viewing satellite detected fault Persian date Esfand 1383 Zarand earthquake, based on radar interferometry method.
30. Nissen, E., Yamini-Fard, F., Tatar, M., Gholamzadeh, A., Bergman, E., Elliott, J. R.Parsons, B. (2010). "The vertical separation of mainshock rupture and microseismicity at Qeshm island in the Zagros fold-and-thrust belt, Iran", Earth and Planetary Science Letters, 296(3-4), 181-194. doi:http://dx.doi.org/10.1016/j.epsl.2010.04.049. [DOI:10.1016/j.epsl.2010.04.049]
31. Nissen, E., Jackson, J., Jahani, S., & Tatar, M. (2014). "Zagros "phantom earthquakes" reassessed-The interplay of seismicity and deep salt flow in the Simply Folded Belt?", Journal of Geophysical Research: Solid Earth. [DOI:10.1002/2013JB010796]
32. R. Azzaro, S. Del Mese, G. Martini, S. Paolini, A. Screpanti, V. Verrubbi, and A. Tertulliani, "Rilievo macrosismico per il terremoto dellisola di Ischia del 21 agosto 2017, Internal Report, doi:10.5281/zenodo.849091.
33. Okada, Y. (1985). Surface deformation due to shear and tensile faults in a half-space. Bulletin of the Seismological Society of America, 75(4), 1135-1154. [DOI:10.1785/BSSA0750041135]
34. Marquardt, D. (1963). An Algorithm for Least-Squares Estimation of Nonlinear Parameters. Journal of the Society for Industrial and Applied Mathematics, 11(2), 431-441. doi:10.1137/0111030. [DOI:10.1137/0111030]
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Karami E, Alizadeh N, sahebi M. Monitoring of ground movement and estimation of earthquake fault parameters using Sentinel-1 data (Case study: Genaveh earthquake). JGST 2023; 12 (3) : 3
URL: http://jgst.issgeac.ir/article-1-1078-en.html


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Volume 12, Issue 3 (3-2023) Back to browse issues page
نشریه علمی علوم و فنون نقشه برداری Journal of Geomatics Science and Technology