Fig. 9
From: A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric data
Posterior results for inversion runs without commonality of shape ratio constraints and variable probability of lithologic changes (Case 2). Posterior results for a–c. Most probable lithology and (d–f) mean bulk density for inversion runs with variable probability of the inversion process proposing lithologic changes: (a, d) 0% probability of lithologic changes (density-only inversion, Case 2a), (b, e) 50% probability of lithologic changes (Case 2b) (c, f 100% probability of lithologic change (Case 2c)