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Published April 13, 2021 | Version 1.0.0
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Data for: Segmentation and Holocene Behavior of the Middle Strand of the North Anatolian Fault (NW Turkey)

Authors/Creators

  • 1. Yacine
  • 2. Julia
  • 3. Stéphane
  • 4. Julien
  • 5. Yann

Contributors

Supervisor:

  • 1. Julia

Description

This dataset is associated to the article "Segmentation and Holocene Behavior of the Middle Strand of the North Anatolian Fault (NW Turkey)" in revision for Tectonics.

It includes the following:

  • A description file, including a list of data files, and a description of how the marker quality score was determined in this study ("Supporting Information.docx")
  • A table summarizing the historical earthquakes in the region of interest ("TableS1.xlsx")
  • A table summarizing the paleoseismic investigations in the region of interest ("TableS2.xlsx")
  • The full horizontal offset retrodeformations ("offsets_X.tif")
  • A table of the offset values measured along the MNAF (TableS3.xlsx")
  • The georeferenced fault map ("MNAF_2021.gml" and "MNAF_2021.xsd")
  • A figure showing examples of vertical slip markers along the MNAF south of Iznik Lake ("FigS1.tif")
  • A figure showing field examples of Late Quaternary faulting along the MNAF ("FigS2.png")
  • A figure showing the results of the automatic fault discretization procedure ("FigS3.png")

Notes

Retrodeformed marker ID is indicated on the left. Columns 1 and 2 show the original morphologies. The fault is drawn in red. Columns 3, 4 and 5 show the retrodeformed morphologies giving the minimum, preferred and maximum offset values respectively. The field "note" of the fault map indicates high confidence (1) and low confidence (0) mapping. Acknowledgements: This work has been supported by the MISTRALS-ENVIMED program (NAFIGEA project), the INSU ALEAS program (France), LabEx OSUG@2020 (Investissements d'avenir - ANR10 LABX56, France), and ANR CE03-2019 Basiliznik-secrets. This study contributes to the IdEx Université de Paris ANR-18-IDEX-0001.

Files

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Additional details

References

  • Ambraseys, N. (2000). The Seismicity of the Marmara Sea Area 1800-1899. Journal of Earthquake Engineering, 4(3), 377–401.
  • Ambraseys, N. N. (2001). Reassessment of earthquakes, 1900–1999, in the eastern Mediterranean and the Middle East. Geophys. J. Int., 145(2), 471–485.
  • Ambraseys, N. (2002), The seismic activity of the Marmara Sea region over the last 2000 years. Bulletin of the Seismological Society of America, 92(1), 1–18.
  • Ambraseys, N. (2009), Earthquakes in the Mediterranean and Middle East. A multidisciplinary study of seismicity up to 1900. Cambridge: Cambridge University Press.
  • Ambraseys, N. & Finkel, C. (1991), Long-term seismicity of Istanbul and of the Marmara Sea region. Terra Nova, 3(5), 527–539.
  • Ambraseys, N. N., and Finkel, C. F. (1995). The Seismicity of Turkey and Adjacent Areas: A Historical Review, 1500–1800, 240 pp., Muhittin Salih Eren, Istanbul.
  • Ambraseys, N. N., and J. Jackson (1998). Faulting associated with historical and recent earthquakes in the eastern Mediterranean region. Geophys. J. Int., 133(2), 390–406.
  • Civico, R., Smedile, A., Pantosti, D., Cinti, F. R., De Martini, P. M., Pucci, S., et al. (2021). New trenching results along the Iznik segment of the central strand of the North Anatolian Fault (Turkey): an integration with preexisting data. Mediterranean Geoscience Reviews. https://doi.org/10.1007/s42990-021-00054-9
  • Dikbas, A., Akyüz, H. S., Meghraoui, M., Ferry, M., Altunel, E., Zabci, C., Langridge, R., Yalciner, C. C. (2018). Paleoseismic history and slip rate along the Sapanca-Akyazi segment of the 1999 Izmit earthquake rupture (MW=7.4) of the North Anatolian Fault (Turkey). Tectonophysics, 738-739, 92-111.
  • Dogan, B. (2010), Kuzey Anadolu Fay Sistemi Güney Kolunun Geyve-Gemlik Arasindaki Kesiminin Morfotektonik, Tektonostratigrafik ve Paleosismolojik Evrimi. (Doctoral dissertation). Istanbul: Istanbul Teknik Üniversitesi.
  • Guidoboni, E., and Comastri, A. (Eds.) (2005). Catalogue of Earthquakes and Tsunamis in the Mediterranean Area From the 11th to the 15th Century, 1037 pp., Ist. Naz. de Geophys. e Vulcanol., Bologna, Italy.
  • Guidoboni, E., Comastri, A., and Traina, G. (1994). Catalogue of ancient earthquakes in the Mediterranean area up to the 10th century. Istituto Nazionale di Geofisica.
  • Honkura, Y. & Isikara, A. M. (1991), Multidisciplinary research on fault activity in the western part of the North Anatolian Fault Zone. Tectonophysics, 193(4), 347–357.
  • Ikeda, Y., Suzuki, Y., Herece, E., Saroglu, F., Isikara, A. M., Honkura, Y. (1991). Geological evidence for the last two faulting events on the North Anatolian fault zone in the Mudurnu Valley, western Turkey. Tectonophysics, 193, 335-345.
  • Klinger, Y., Sieh, K., Altunel, E., Akoglu, A., Barka, A., Dawson, T., Gonzalez, T., Meltzner, A., Rockwell, T. (2003). Paleoseismic Evidence of Characteristic Slip on the Western Segment of the North Anatolian Fault, Turkey. Bulletin of the Seismological Society of America, 93(6), 2317-2332.
  • Özalp, S., Emre, Ö., & Dogan, A. (2013), The segment structure of southern branch of the North Anatolian Fault and paleoseismological behaviour of the Gemlik fault, NW Anatolia. Bulletin of MTA, 147, 1–17.
  • Rockwell, T., et al. (2009). Palaeoseismology of the North Anatolian Fault near the Marmara Sea: Implications for fault segmentation and seismic hazard. In: Reicherter, K., Michetti, A. M., and Silva, P. G. (Eds), Palaeoseismology: Historical and Prehistorical Records of Earthquake Ground Effects for Seismic Hazard Assessment. Geol. Soc. Spec. Publ., 316(1), 31-54.