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Fig. 8 | Geothermal Energy

Fig. 8

From: Advances in the modeling of the Iberian thermal lithosphere and perspectives on deep geothermal studies

Fig. 8

Differences in temperature distribution between thermal modeling based on Bayesian geophysical–petrological inversion of surface waves, surface heat flux, elevation, and geoid anomalies (Fullea et al. 2021), and on geoid and elevation inversion integrated with 3D inversion gravity modeling (Torne et al. 2015), at 5 km crustal depth (a), at 10 km (b), at 20 km (c) and at Moho depth (d)

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