EGU25-14332, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-14332
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 29 Apr, 10:45–12:30 (CEST), Display time Tuesday, 29 Apr, 08:30–12:30
 
Hall X3, X3.78
Luminescence Surface Exposure Dating and Paleoseismic Insights from the Kuşadası Fault Zone, Western Türkiye
Mustafa Softa1,3, Eren Şahiner2, Joel Q.G. Spencer3, Hasan Sözbilir1, Mehmet Yüksel4, Mehmet Utku5, Naki Akçar6, Sabah Kırallı1, Büşra Yerli1, Recep Çakır7, Fatih Mehmet Büyüktopçu1, and Fırat Deniz4
Mustafa Softa et al.
  • 1Dokuz Eylül University, Dept. of Geology, Izmir, Türkiye (mustafa.softa@deu.edu.tr)
  • 2Ankara University, Luminescence Dating Research Laboratory, Earth Sciences Application and Research Center, Ankara, Türkiye
  • 3Kansas State University, Faculty of Engineering, Geology Engineering, Manhattan, Kansas, United States
  • 4Çukurova University, Faculty of Science and Letters, Physics, Adana, Türkiye
  • 5Dokuz Eylül University, Faculty of Engineering, Geophysical Engineering, İzmir, Türkiye
  • 6University of Bern, Institute of Geology, Bern, Switzerland
  • 7Washington State Department of Natural Resources, Washington Geological Survey, Olympia, WA, United States

Exposure dating has become a critical tool in addressing specific geoscientific challenges, including glaciology, active fault studies, and environmental reconstructions. Cosmogenic exposure dating (e.g., 36Cl) and luminescence surface exposure dating are widely used techniques, often complementing each other. In active tectonic studies across Türkiye, cosmogenic 36Cl dating has been applied extensively to active faults to elucidate paleoseismic histories and slip rates. Although luminescence surface exposure dating is relatively new in this context, its initial applications along the Manisa Fault in Western Türkiye have shown promising results. In this study, we focus on the Kalafat and Yavansu faults within the Kuşadası Fault Zone, which is considered the eastern continuation of the Samos Fault that ruptured during the 30 October 2020 earthquake. This region, characterized by N-S extensional tectonics with horst-graben structures and normal faulting, offers well-preserved fault scarps that serve as natural laboratories for exposure dating.

Preliminary luminescence depth profiling of scarp samples and optically stimulated luminescence (OSL) dating of associated colluvial wedges provide valuable insights into the paleoseismic history of these faults: (i) Luminescence profiling revealed stable signal limits at ~6 mm, with intensity increasing with depth; (ii) Calibration against prior cosmogenic dating yielded uppermost ages of ~15 ka for KF and ~8 ka for YF; (iii) OSL dating of colluvial wedge bases produced ages of 16.56 ± 1.77 ka for KF and 14.45 ± 0.74 ka for YF. These results indicate significant seismic activity along both faults during the Late Pleistocene, consistent with regional tectonic processes. This research underscores the utility of integrating luminescence surface exposure techniques with cosmogenic methods for refining paleoseismic chronologies. This study is fully supported by the Dokuz Eylül University Scientific Research Project (Project No. FBA-2023-3042).

How to cite: Softa, M., Şahiner, E., Spencer, J. Q. G., Sözbilir, H., Yüksel, M., Utku, M., Akçar, N., Kırallı, S., Yerli, B., Çakır, R., Büyüktopçu, F. M., and Deniz, F.: Luminescence Surface Exposure Dating and Paleoseismic Insights from the Kuşadası Fault Zone, Western Türkiye, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-14332, https://doi.org/10.5194/egusphere-egu25-14332, 2025.