Fig. 10
From: A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric data
Posterior results for an inversion run with moderate commonality constraint (Case 3a). Posterior probability of (a–c) hyaloclastite, (d–f), lava flow, and (g–i) most probable lithology and (k–m) mean bulk density. Letters at the top of the different sections indicate proximity to different sub-areas of the Krafla field (V Vitismor, Lb Leirbotnar, Hh Hvitholar, Hv Hveragil, Vh Vesturhlí\(\eth\)ur, Ln Leirhnjúkur, Su Su\(\eth\)urhlí\(\eth\)ur)