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Azimuthal anisotropy in the wider Vienna basin region: a proxy for the present-day stress field and deformation

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Academic year: 2021

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Figure

Figure 1. Tectonic sketch map of the study area illustrating the lateral extru- extru-sion of blocks (the southeastern half), accommodated by the major fault  sys-tems and subsequent formation of the Vienna Basin in the Alpine-Carpathian transition zone
Figure 2. Interstation geometry for all available station pairs (a) and the station pairs remaining after selection criteria applied during group velocity measurements for different periods (b–f)
Figure 3. Directional dependence (2 θ -terms) of group velocities for measured (a), modelled (b), and residual (c) group velocities
Figure 4. Regionalization of fast orientations for measured (a, e), modelled (b, f) and residual group velocities (c, g) in a grid of 2 ◦ -cells, overlapping with 85 per cent at 5 s (top row) and 20 s (bottom row)
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