Journals / NATURENGS / 2025 / Volume: 6 Issue: 2

Relationship between Earthquake Damage Patterns Observed in Doğanşehir (Malatya) and Local Fault Geometry and Soil Conditions

Çiğdem Ceylan(MALATYA TURGUT ÖZAL ÜNİVERSİTESİ)0000-0002-5961-3085
Journal
NATURENGS
Pages
—
Publication Date
2025-12-30
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The findings indicate that the neighborhoods with the highest damage rates (Polat: 93.11%; Doğu: 66.0%) were located on rocky ground (Polat Granitoid), rather than on alluvial ground, contrary to expectations.

📌 3 Key Takeaways

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Objective & Hypothesis:This study presents a detailed case analysis of the seismotectonic and ground-based causes of destruction in the Doğanşehir (Malatya) district following the February 6, 2023, Pazarcık (Mw: 7.7) and Elbistan (Mw: 7.6) earthquakes.
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Key Findings & Data:Located close to the East Anatolian Fault Zone and at the intersection of the Sürgü, Malatya, and Doğanşehir faults, the district sustained severe damage to more than 7,500 buildings.
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Conclusion & Impact:The findings indicate that the neighborhoods with the highest damage rates (Polat: 93.11%; Doğu: 66.0%) were located on rocky ground (Polat Granitoid), rather than on alluvial ground, contrary to expectations.
🔬Design:Research Article
📍Scope:2023 Verileri
⚙️Variables:Earthquake · Near-Fault Effect · Damage Distribution

Abstract

This study presents a detailed case analysis of the seismotectonic and ground-based causes of destruction in the Doğanşehir (Malatya) district following the February 6, 2023, Pazarcık (Mw: 7.7) and Elbistan (Mw: 7.6) earthquakes. Located close to the East Anatolian Fault Zone and at the intersection of the Sürgü, Malatya, and Doğanşehir faults, the district sustained severe damage to more than 7,500 buildings. The analysis is based on field observations, official damage data, geological maps, and aftershock distributions. The findings indicate that the neighborhoods with the highest damage rates (Polat: 93.11%; Doğu: 66.0%) were located on rocky ground (Polat Granitoid), rather than on alluvial ground, contrary to expectations. This observation highlights that the primary factor determining damage severity can be the absolute proximity to the ruptured Doğanşehir Fault (near-fault effect), rather than the ground condition itself. The high damage in Yenimahalle and Karşıyaka, located on alluvial ground, is associated with stress concentrations occurring at the intersection of the Malatya and Sürgü Faults. This case study demonstrates that a single factor cannot explain the destruction; a combination of local fault rupture, fault proximity, fault intersection effects, and structural vulnerabilities played a combined role. The results underscore the critical importance of detailed mapping of local faults, identification of fault-exclusion zones, and microzonation studies for earthquake risk management in comparable tectonic settings.

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Cite This Article

Ceylan, Ç. (2025). Relationship between Earthquake Damage Patterns Observed in Doğanşehir (Malatya) and Local Fault Geometry and Soil Conditions. NATURENGS, Volume: 6 Issue: 2. https://doi.org/10.46572/naturengs.1821725

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References (44)

  1. Google Maps. (n.d.). Retrieved from https://www.google.com/maps/@38.3297582,38.205684,13604m/data=!3m1!1e3?entry=ttu&g_ep=EgoyMDI1MTEwNC4xIKXMDSoASAFQAw%3D%3D
  2. https://www.nufusune.com/dogansehir-ilce-nufusu-malatya
  3. Şengör, AC, & Yilmaz, Y., (1981). Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics 75 (3-4), 181-241.
  4. Hempton, MR., (1985). Structure and deformation history of the Bitlis suture near Lake Hazar, southeastern Turkey. Geological Society of America Bulletin, 96 (2), 233-243.
  5. Bulut, F., Bohnhoff, M., Eken, T., Janssen, C., Kılıç, T., & Dresen, G., (2012). The East Anatolian Fault Zone: Seismotectonic setting and spatiotemporal characteristics of seismicity based on precise earthquake locations. Journal of Geophysical Research: Solid Earth, 117. (B7).
  6. Duman, TY. & Emre, Ö., (2013). The East Anatolian Fault: geometry, segmentation, and jog characteristics. Geological Society, London, Special Publications, 372 (1), 495-529.
  7. Demirtaş, R., (1998). Seismic Gaps in Turkey and the June 27, Ceyhan (Adana) Earthquake (Ms=6.3).
  8. Ceylan, C., (2020). Seismicity of Malatya Province in Terms of Settlement Area and Ground Relationship. 2nd International Malatya Applied Sciences Congress. (Full Text Paper / Oral Presentation) (Publication Date: 24.04.2020 / ISBN: 978-605-7811-58-5).
  9. Emre, Ö., Duman, TY, Özalp, S., Şaroğlu, F., Olgun, Ş., Elmacı, H., & Çan, T., (2018). Active fault database of Turkey. Bulletin of Earthquake Engineering, 16(8), 3229-3275.
  10. Li, Y., Huang, L., Ding, R., Yang, S., Liu, L., Zhang, S., & Liu, H., (2021). Coulomb stress changes associated with the M7. 3 Maduo earthquake and implications for seismic hazards. Natural Hazards Research, 1(2), 95-101.
  11. Dokuz Eylül University. February 6, 2023, 04:17, Mw=7.7, H=9 km Pazarcık (Kahramanmaraş) Earthquake. February 6, 2023, 13:24, Mw=7.6, H=7 km Elbistan (Kahramanmaraş) Earthquake. February 20, 2023, 20:04, Mw=6.4, H=22 km Defne (Hatay) Earthquake. Earthquake Report, 03.03.2023.
  12. Dedeoğlu, İ. Ö., Yetkın, M., & Calayır, Y., (2020). January 24, 2020 Sivrice-Elazığ earthquake: assessment of seismic characteristics of earthquake, earthquake territory and structural performance of reinforced concrete structures. Sakarya University Journal of Science, 26(5), 892-907.
  13. Ambraseys, NN., (1989). Temporary seismic quiescence: SE Turkey. Geophysical Journal International 96(2), 311-331.
  14. https://www.mta.gov.tr/v3.0/arastirmalar/kesfedilen-maden-sahalari#12
  15. Önal, M., Şahinci, A., & Gözübol, A. M., (1986). Hydrogeological Investigation of Yesilyurt-Celikhan (Malatya-Adıyaman) Area. Geological Engineering, 29, 5-12.
  16. Önal, M., (1995). Miocene stratigraphy and lignite potential of the northern part of the Malatya graben basin, East Anatolia-Turkey: International Earth Sciences Colloquium on the Aegean region (IESCA-1995), 607 – 621.
  17. Yılmaz, Y., Yiğitbaş, E. & Genç, Ş. C., (1993). Ophiolitic and metamorphic assemblages of southeast Anatolia and their significance in the geological evolution of the orogenic belt. Tectonics, 12(5), 1280-1297.
  18. Yazgan, E., Michard, A., Whitechurch, H., & Montigny, R., (1983). Le Taurus de Malatya (Turquie orientale) élément de la suture sud-téthysienne. Bulletin de la Société géologique de France, 25, 59-69
  19. Önal, A., & Bingöl, A.F., (1997). Geology of the west of Doğanşehir (Malatya). Selçuk University, Faculty of Engineering and Architecture Journal, 12, 63-75.
  20. Önal, A., & Altunbey, M., (1999). Skarn formations and associated iron mineralizations in the Dedeyazı-Çavuşlu (Doğanşehir/Malatya) region. Turkish Geological Bulletin, 42(1), 15-27.
  21. Palutoğlu, M., & Tanyolu, E., (2006). Seismicity of Elazığ city center residential area. Fırat University Journal of Science and Engineering, 18(4), 577-588.
  22. http://yerbilimleri.mta.gov.tr/anasayfa.aspx
  23. Kaymakci, N., Inceoez, M., & Ertepinar, P., (2006). 3D-architecture and Neogene evolution of the Malatya Basin: inferences for the kinematics of the Malatya and Ovacık fault zones. Turkish Journal of Earth Sciences, 15(2), 123-154.
  24. Westaway, ROB, & Arger, JAN (2001). Kinematics of the Malatya–Ovacik fault zone. Geodinamica Acta, 14 (1-3), 103-131.
  25. http://udim.koeri.boun.edu.tr/zeqmap/hgmmap.asp
  26. Acarel, D., Cambaz, MD, Turhan, F., Mutlu, AK, & Polat, R., (2019). Seismotectonics of Malatya Fault, Eastern Turkey. Open Geosciences, 11(1), 1098-1111.
  27. https://tdth.afad.gov.tr/
  28. Taymaz, T., Eyidog̃an, H., & Jackson, J., (1991). Source parameters of large earthquakes in the East Anatolian Fault Zone (Turkey). Geophysical Journal International, 106(3), 537-550.
  29. http://www.koeri.boun.edu.tr/sismo/2/deprem-bilgileri/buyuk-depremler/
  30. Malatya Turgut Ozal University. February 6, 2023, Pazarcik (Mw 7.7) and Elbistan (Mw 7.6) Earthquakes Preliminary Assessment Report, 14.03.2023.
  31. https://www.afad.gov.tr/
  32. https://deprem.afad.gov.tr/last-earthquakes.html
  33. https://earthexplorer.usgs.gov
  34. Middle East Technical University. February 6, 2023 Kahramanmaraş-Pazarcık Mw=7.7 and Elbistan Mw=7.6 Earthquakes Preliminary Assessment Report, 20.02.2023.
  35. https://www.hmb.gov.tr/haberler/2023-kahramanmaras-ve-hatay-depremleri-raporu
  36. http://www.malatya.gov.tr/08052023-deprem-durum-cizelgesi
  37. Wikipedia. (n.d.). Türkiye’deki depremler listesi. https://tr.wikipedia.org/wiki/Türkiye%27deki_depremler_listesi
  38. Yıldız, Ö. & Kına, C., (2023). Geotechnical and structural investigations in Malatya Province after Kahramanmaraş Earthquake on February 6, 2023. Bitlis Eren University Journal of Science, 12(3), 686-703.
  39. Yıldız, Ö. & Çabalar, AF., (2024). Analyzing Seismic Impact Across Regions: A Comprehensive Study of the Pazarcık and Elbistan Earthquakes in Türkiye (February 6, 2023). Journal of African Earth Sciences 105463.
  40. https://hasartespit.csb.gov.tr/
  41. Yıldız, Ö, Zeybek, A., & Sönmezer, YB., (2024). Investigation of the earthquake-induced liquefaction and seismic amplifications after the Pazarcık (Mw 7.7) and Elbistan (Mw 7.6) earthquakes. Environmental Earth Sciences, 83(21), 1-21.
  42. Yıldız, Ö, (2024). Integrated GIS-Based Mapping and ANFIS Modeling for Seismic and Geotechnical Characterization of Soil Properties. KSCE Journal of Civil Engineering, 1-14
  43. Yıldız, Ö, (2022). Seismic site characterization of Battalgazi in Malatya, Turkey. Arabian Journal of Geosciences, 15(9), 867.
  44. Yıldız, Ö., (2023). Influence of input motion and surface layer properties on seismic siteresponse: A stochastic simulation method–based MLR model. Near Surface Geophysics, 21(3), 195-216.