Synthetic Seismic Reflection Modelling in a Supercritical Geothermal System: An Image of the K-Horizon in the Larderello Field (Italy)

Figure 2

Geological cross section of the study area (see the X-X′ trace in Figure 1 for the location) (modified after [10]). The contact metamorphic isograde, main seismic horizons (H and K), isotherms, and radiometric ages are reported. Note that this illustration represents one of the various geological frameworks proposed for the study area. Table 1 mentions the proposed alternative interpretations of the K-horizon.