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Table 2 1D velocity model used in the study

From: Full, constrained and stochastic source inversions support evidence for volumetric changes during the Basel earthquake sequence

Thickness (km) Vp (km/s) Vs (km/s) Density Qp Qs
0.20 1.80 1.00 2.30 50 25
0.70 3.40 2.00 2.40 50 25
0.35 4.20 2.70 2.50 250 100
0.75 5.20 2.90 2.60 250 100
1.00 5.60 3.25 2.85 250 100
1.70 5.95 3.45 2.85 500 250
90.00 5.95 3.45 2.85 500 250
  1. The P-wave model corresponds to Model 2 of Deichmann and Ernst (2009). The S-wave model is adapted from the reference 1D model of Ripperger et al. (2009)