1.
ORLICKÝ O. Field-reversal versus self-reversal hypothesis: The Ti-rich titanomagnetite bearing basalts and their partly self-reversed partial thermoremanent magnetization induced in the laboratory field. Contrib. Geophys. Geod. [Internet]. 2021 May 6 [cited 2026 Feb. 4];36(2):171-88. Available from: https://journals.savba.sk/index.php/cgg/article/view/5013