t from Step 3 which comprises parts from three different geologic faults, A, B, and C; [0043]FIG. 19 is a 3-D view of the same fault object in FIG. 18, after automated separation of into three separate fault objects; [0044]FIG. 20 is a vertical map-like view of fault pattern derived from Step 4 of the fault autopicking process; [0045]FIG. 21 is an image illustrating a fault pattern oriented in 3-D