Fig. 10From: Polyphase movement on the Lavanttal Fault Zone (Eastern Alps): reconciling the evidence from different geochronological indicatorsSchematic cross sections (not to scale) for the evolution of the LFZ and the adjacent Koralm Massif and Styrian Basin during Miocene times. HePRZ He partial retention zone; APAZ apatite partial annealing zone; ZPAZ zircon partial annealing zoneBack to article page