Fig. 7From: The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust beltSynthetic waveform modelling at stations CHE (distance ~ 70 km) and FELD (distance ~ 80 km). The right panel shows a zoom-in view around the P arrival time of the panel on the left. In each panel the top trace (green)represents the vertical component of the ML 3.2 event of 2000 recorded at both CHE and FELD, respectively, whereas the bottom traces are synthetic seismograms for focal depths 0–6 km. Note how the sPmP is not visible in the data, matching the synthetic seismograms for depth shallower than 1 kmBack to article page