ORLICKÝ, Oto. Field-reversal versus self-reversal hypothesis: Alterations of the Fe-Ti magnetic minerals and an origin of reversed RM of volcanics. Contributions to Geophysics and Geodesy, [S. l.], v. 38, n. 2, p. 187–208, 2008. Disponível em: https://journals.savba.sk/index.php/cgg/article/view/5084. Acesso em: 4 feb. 2026.