Fig. 12From: A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric dataEffect of strength of shape ratio constraint on uncertainty of posterior results (Case 3d–f). Posterior results for (a–c) most probable lithology and (d–f) information entropy, for inversion runs with (a, d) smoother shape ratio constraint (Case 3d), (b, e) similar shape ratio constraint (Case 3e), (c, f) rougher shape ratio constraint (Case 3f). Results are shown along Section 2Back to article page