Fig. 12From: Influence of depth, temperature, and structure of a crustal heat source on the geothermal reservoirs of Tuscany: numerical modelling and sensitivity studyVertical cross-sections along A–A′ (top) and B–B′ (bottom) (see Fig. 9 for their positions) showing Darcy velocity (arrows) within the Burano unit. The magnitude of a reference arrow is given at the top-left corner. The shaded areas represent reservoir layers of high permeability. The velocity in the deep geothermal reservoir within the Farma unit is not shown to avoid clutter. The colouring represents temperatureBack to article page