Fig. 4From: Polyphase movement on the Lavanttal Fault Zone (Eastern Alps): reconciling the evidence from different geochronological indicatorsSchematic lithologs of parts of drill cores KB-D13/02 and KB-D12/02, with the sampling sites for 40Ar/39Ar dating of muscovite and the corresponding integrated plateau ages. For location of sampled drilling sites, see Fig. 2. Samples from fault cores are highlighted. FC fault core, DZ damage zone, HR host rockBack to article page