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

Figure 11

(a) Velocity model, named model 2-B (see Figure 10(b)). (b) Studied segment of the CROP-18A stacked section (see Figure 6(b)). (c) The figure shows the time-migrated section of the CROP-18A data, reported in Figure 11(b), obtained through the calibrated velocity model shown in Figure 11(a). The time migrated section improves event focusing and reduces diffracted events. Note the high focusing of the bulge-like structure between CMPs 749 and 849 and the two events bordering the bulge structure and dipping southward and northward.