Fig. 9
From: Ground motions induced by pore pressure changes at the Szentes geothermal area, SE Hungary
source is outlined with grey. Cm values that lie within the grey interval indicate reasonable estimates for the decompaction coefficients of the reservoir system
Decompaction coefficient associated with sources 1 as a function of reservoir pressure, with constant reservoir heights of 200, 400 and 600 m. The interval with reasonable values for pressure change based on water level observations from the locations of the corresponding