Fig. 6From: A new magnetostratigraphic framework for the Lower Miocene (Burdigalian/Ottnangian, Karpatian) in the North Alpine Foreland BasinRepresentative examples of the IRM component analysis (Kruiver et al. 2001). a Druisheim core: wide DP typical for detrital magnetite. b Pfyffrüti section: two components, detrital magnetite and hematite. c Druisheim core: narrow DP (0.2) typical for biogenic magnetiteBack to article page