ORLICKÝ, Oto. Field-reversal versus self-reversal hypothesis: Different intensities of TRM of the reversely magnetized natural basalts and those of the same origin of artificial samples magnetized in laboratory. Contributions to Geophysics and Geodesy, [S. l.], v. 36, n. 1, p. 35–48, 2021. Disponível em: https://journals.savba.sk/index.php/cgg/article/view/4954. Acesso em: 4 feb. 2026.