ORLICKÝ O. 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. Contrib. Geophys. Geod. 2021;36(1):35-48. Accessed February 4, 2026. https://journals.savba.sk/index.php/cgg/article/view/4954