Fig. 2From: Coda wave interferometry during the heating of deep geothermal reservoir rocksEvolution of the sample temperature with time in the simulation. The temperature is computed at the middle of the sample using Code_Aster, while temperature is increased step by step from 20 to 450 °C by 10 °C steps. Right inset shows the progressive diffusion of temperature during one step of the deformation process in the simulation (from 200 to 210 °C)Back to article page