Figure 17From: Tracing of paleo-shear zones by self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes The KTB Anomaly I: inversion results retrieved from various initial guesses. The measured data (redrawn from Figure two(a) of Stoll et al.1995) and the predicted response are shown in open and solid circles, respectively.Back to article page