GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 3.1 GNGTS 2024 generally lower than 1 (Fig. 2 – top panel). For sake of completeness, the probabilistc inversion was Fig. 1 – Horizontal slices presentng the inversion outcomes derived from the Frequency-Domain Electromagnetc Inducton (FDEM) data collected across the Danta peatland in Italy. Each row shows the resistvity model with maximum likelihood and the probability of encountering peat or clay. Rows (a-b) depict these models and probabilites at depths of 3.0 m and 7.0 m respectvely. In the third column, above the peat probability, the fgure displays the profle's locaton shown in Figure 2 (highlighted in bright green), along with the positons of associated boreholes marked by red X.