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Swiss Journal of Geosciences
Fig. 2 | Swiss Journal of Geosciences

Fig. 2

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

Fig. 2

Seismograms of event 113 (ML 2.5) recorded at Stations OTTER (a) and SBIS (b). Top panels show unfiltered acceleration seismograms, bottom panels show bandpass filtered (0.5–3 Hz) displacement seismograms. ‘OT’ corresponds to origin time. Note the impulsive P-wave arrival visible in the unfiltered data. In the bandpass filtered data, the horizontally polarized S-wave dominates the seismograms

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