1.
ORLICKÝ O. Field-reversal versus self-reversal hypothesis: Alterations of the Fe-Ti magnetic minerals and an origin of reversed RM of volcanics. Contrib. Geophys. Geod. [Internet]. 2008 Jun. 30 [cited 2026 Feb. 4];38(2):187–208. Available from: https://journals.savba.sk/index.php/cgg/article/view/5084