Articles | Volume 10, issue 2
https://doi.org/10.5194/se-10-363-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-363-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Near-surface structure of the North Anatolian Fault zone from Rayleigh and Love wave tomography using ambient seismic noise
School of Earth and Environment, University of Leeds, LS2 9JT Leeds, UK
now at: Institute of Seismology, University of
Helsinki, 00014 Helsinki, Finland
Sebastian Rost
School of Earth and Environment, University of Leeds, LS2 9JT Leeds, UK
Gregory A. Houseman
School of Earth and Environment, University of Leeds, LS2 9JT Leeds, UK
Gregor Hillers
Institut des Sciences de la Terre, Université Grenoble-Alpes,
38041 Grenoble, France
now at: Institute of Seismology, University of
Helsinki, 00014 Helsinki, Finland
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- Structure of the northwestern North Anatolian Fault Zone imaged via teleseismic scattering tomography S. Rost et al. 10.1093/gji/ggab265
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- Imaging the Crustal and Upper Mantle Structure of the North Anatolian Fault: A Transmission Matrix Framework for Local Adaptive Focusing R. Touma et al. 10.1029/2023JB026704
- The Influence of the North Anatolian Fault and a Fragmenting Slab Architecture on Upper Mantle Seismic Anisotropy in the Eastern Mediterranean T. Merry et al. 10.1029/2021GC009896
- Evaluation of local soil conditions with 1D nonlinear site response analysis of Arifiye (Sakarya District), Turkey A. Silahtar 10.1007/s11069-022-05695-z
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- Phase-velocity inversion from data-based diffraction kernels: seismic Michelson interferometer M. Chmiel et al. 10.1093/gji/ggaa512
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 14 Dec 2024
Short summary
We constructed a seismic velocity model of the North Anatolian Fault in Turkey. We found that the fault is located within a region of reduced seismic velocity and skirts the edges of a geological unit that displays high seismic velocity, indicating that this unit could be stronger than the surrounding material. Furthermore, we found that seismic waves travel fastest in the NE–SW direction, which is the direction of maximum extension for this part of Turkey and indicates mineral alignment.
We constructed a seismic velocity model of the North Anatolian Fault in Turkey. We found that...