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]. 2008Jun.30 [cited 2024Nov.24];38(2):187–208. Available from: https://journal.geo.sav.sk/cgg/article/view/271