Fig. 5From: Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines(modified from Goswami et al. 2013)Two-dimensional model of a fault propagating fold (Suppe and Medwedeff 1990). According to the model, a fold grows at the tip of a propagating thrust fault. The steep limb of the fold dips on the opposite direction relative to the propagating faultBack to article page