A new original conception in rock magnetism, paleomagnetism and geomagnetism: An origin of the reversed magnetization of rocks on Earth
So far the field-reversal theory has been accepted to account for the reversed remanent magnetization (RM) of rocks on the Earth. Orlický (2014) revealed a frequent occurrence of the antiferromagnetic (AFM) Fe-Ti oxides in the rocks. Now I have renamed these minerals as the Fe-Ti ferrimagnetic-antif...
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| Format: | Article |
| Language: | English |
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Earth Science Institute, Slovak Academy of Sciences, Slovakia
2018-03-01
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| Series: | Contributions to Geophysics and Geodesy |
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| Online Access: | https://journal.geo.sav.sk/cgg/article/view/178 |