Fig. 5
From: Thin-sheet electromagnetic modeling of magnetovariational data for a regional-scale study
Conductance map from the inversion of magnetovariational sounding (MVS) data after the rediscretization of blocks to 25 by 25 km. The interpreted conductivity anomalies are the: Central Finland Granitoid Complex (CFGC), Southern Finland conductivity anomaly (SFI),Tampere Belt (TB), Bothnian Belt (BB), Vaasa Dome or Vaasa Granitoid Complex (VGC), Oulu (OUL), Outokumpu (OKU), and Lake Ladoga (LLA) anomalies, and the Karelian Domain (KAD)