Fig. 2From: Influence of depth, temperature, and structure of a crustal heat source on the geothermal reservoirs of Tuscany: numerical modelling and sensitivity studySimplified stratigraphic pile of the Monte Amiata area. Subdivisions of the Tuscan units and the metamorphic complex are omitted, as they are not considered in the model. Note that the K horizon does not represent a lithological boundaryBack to article page