Fig. 4
From: Clockwise vertical-axis rotation in the West Vardar zone of Serbia: tectonic implications
Data from the Cretaceous sediments of the wider Rudnik Mts. area regarding the identification of magnetic minerals (method by Lowrie 1990). From top to bottom: IRM acquisition, thermal demagnetization of the three-component IRM and its normalized version, susceptibility during heating. The components of the IRM were acquired in fields of 2.8 T (squares), 0.8 T (full circles) and 0.12 T (open circles)