ORLICKÝ, Oto. The self-reversal origin of the reversed remanent magnetization in the igneous rocks containing the oxidized Fe-Ti oxide solid solutions. Contributions to Geophysics and Geodesy, [S. l.], v. 41, n. 1, p. 19–44, 2011. DOI: 10.2478/v10126-011-0002-3. Disponível em: https://journal.geo.sav.sk/cgg/article/view/46. Acesso em: 3 aug. 2025.