Fig. 14
From: A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric data
Effect of considering hyaloclastite alteration and low-density intrusion on posterior results (Case 5a). Posterior results for most probable lithology assuming (a) prior properties of hyaloclastite assuming all data (Course 4a), (b) altered hyaloclastites (Course 5a), (c) altered hyaloclastites and a low-density intrusion beneath the main upflow (Case 5b), for an inversion also assuming a moderate commonality constraint and rougher shape ratio constraint. Results are shown along Section 3