Fig. 4From: Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines(top) Topographic cross section and (bottom) interpreted CDP stacked section of the Napo seismic line showing that the NBF exhibits vertical segmentation attributed to a lithologic contact between the Middle Miocene sediments and the younger alluvial deposits. Vertical exaggeration for the topographic cross section is ×5, while the seismic profile has no vertical exaggerationBack to article page