Fig. 1From: Fluid-induced seismicity: comparison of rate- and state- and critical pressure theory Left panel shows the flow rate at the injection point with two cycles peaking after 50 and 140 h with 20 l/s maximum amplitude; right panel show pressure at 200 (blue), 300 (green), and 400 (black) m calculated with a diffusion constant of \(D = 0.1\) m2/s. Note the shift in pressure peaks towards higher values and the progressively smaller peak to trough pressure relationBack to article page