ORLICKÝ, Oto. “The Ionic Reordering in Fe-Ti Ferrimagnetics As a Dominant Source of the Reversed RM in Basaltic Rocks”. Contributions to Geophysics and Geodesy 39, no. 1 (March 1, 2009): 55-82. Accessed November 24, 2024. https://journal.geo.sav.sk/cgg/article/view/9.