Figure 7From: Tracing of paleo-shear zones by self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes Model 2: noise-free data. Obtained inversion results (top panel). The observed data and predicted response are coincident with each other. Evolution of the normalized misfit of the SD and GN methods (middle panel). Evolution of the objective functional of the SD and GN methods (bottom panel).Back to article page