(1)
ORLICKÝ, O. The Self-Reversal Origin of the Reversed Remanent Magnetization in the Igneous Rocks Containing the Oxidized Fe-Ti Oxide Solid Solutions. Contrib. Geophys. Geod. 2011, 41 (1), 19-44. https://doi.org/10.2478/v10126-011-0002-3.