Figure 15From: Tracing of paleo-shear zones by self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes Model 4 over truncated from both the left and right : noise free. Inversion results (top panel). Behavior of the normalized misfit and objective functional of the SD method (middle panel) and the GN method (bottom panel). The observed and predicted data shown in open and solid circles, respectively, are coincident with each other.Back to article page