Inferring Hydraulic Pressure Changes from Induced Seismicity Observations: Three Showcases from Geothermal Reservoirs

Figure 15

Percentage of maximum cumulative fluid pressure change for different stress drop models as a function of the maximum number of repeated slips for the three geothermal projects mentioned here (St. Gallen, Paralana, Habanero#1-restimulation) and the Habanero#4-stimulation analysed in Baisch [5].