Published September 12, 2021 | Version 1.2.0
Dataset Open

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)" published in Tectonics (https://doi.org/10.1029/2021TC006870).

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

FigS1.tif

Files (218.9 MB)

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Additional details

Related works

Is supplement to
Journal article: 10.1029/2021TC006870 (DOI)

References

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  • 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.
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  • 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.