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, [S. l.], v. 39, n. 1, p. 55–82, 2009. Disponível em: https://journals.savba.sk/index.php/cgg/article/view/5101. Acesso em: 4 feb. 2026.