Fig. 13
From: A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric data
Effect of strength of assumed measurement error on uncertainty of posterior results (Case 4). Posterior results for (a–b) most probable lithology and (c–d) information entropy, for inversion runs with assumed measurement error of (a, b) 0.1 mGal (Case 4a) or (b, d) 0.5 mGal (Case 4b), for inversions also assuming a moderate commonality constraint and rougher shape ratio constraint. Results are shown along Section 3