Figure 27From: Tracing of paleo-shear zones by self-potential data inversion: case studies from the KTB, Rittsteig, and Grossensees graphite-bearing fault planes The Grossensees anomaly (profile \(\boldsymbol {B \; \widetilde B}\) shown in Figure 25 ): inversion results retrieved from various initial guesses. The measured data and the predicted response are shown in open and solid circles, respectively.Back to article page