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Fig. 6 | Geothermal Energy

Fig. 6

From: Influence of depth, temperature, and structure of a crustal heat source on the geothermal reservoirs of Tuscany: numerical modelling and sensitivity study

Fig. 6

Determination of the rock component shale and siliciclastic matrix, as well as water (i.e. porosity) from the log of one of the boreholes (Borehole 1; see Fig. 3 for its location) and derived thermal conductivities of the Farma formation. In addition, the corresponding thermal conductivities measured on cuttings are shown (black dots)

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