Thin-Sheet Inversion Modeling of Geomagnetic Deep Sounding Data Using MCMC Algorithm
Figure 6
Conductance map from inversion of GDS data with initial block size (a) and after rediscretization of blocks (b). Interpreted anomalies include West Carpathian anomaly (WCA), Bohemian Massif anomaly (BMA), Moravian-Silesian lineament (MSL), and Labe lineament (LL).
