ORLICKÝ, Oto. 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. Contributions to Geophysics and Geodesy, [S. l.], v. 36, n. 2, p. 171–188, 2021. Disponível em: https://journal.geo.sav.sk/cgg/article/view/325. Acesso em: 17 aug. 2025.