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Swiss Journal of Geosciences
Fig. 11 | Swiss Journal of Geosciences

Fig. 11

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

Fig. 11

Time evolution of the earthquake source parameters. a Variation of the absolute isotropic component found for the 28 earthquakes between December 2006 and May 2007. b Moment magnitude vs time. The dots are color-coded by the corresponding isotropic component. No evidence of magnitude dependence of the isotropic changes is observed. c Temporal change of the downhole pressure in kPa (red) measured at the injection site and of the injection flow rate (l/min) compared to earthquake’s occurrence. Dot color gives the absolute isotropic component (colorscale in b), and dot size is proportional to ML

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