Fig. 16From: Influence of rheologically weak layers on fault architecture: insights from analogue models in the context of the Northern Alpine Foreland Basina Line drawing of time-migrated seismic section (NRGS84-407) across the Smørbukk structure, Norwegian North Sea (modified after Withjack et al., 1990). AAPG ©1990, reprinted by permission of the AAPG whose permission is required for further use. b Sketch of slip partitioning that occurred during the 2016 Kumamoto earthquake. Modified after Toda et al. (2016)Back to article page