The ionic reordering in Fe-Ti ferrimagnetics as a dominant source of the reversed RM in basaltic rocks
The basalts of the Pleistocene to Quaternary age from southern part of Slovakia were investigated. These are the basalts containing predominantly the titano- maghemites (Ti-Mgh-es) which carry the reversed remanent magnetization (RM). The partial thermoremanent magnetization (PTRM)...
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| Format: | Article |
| Language: | English |
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Earth Science Institute, Slovak Academy of Sciences, Slovakia
2009-03-01
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| Series: | Contributions to Geophysics and Geodesy |
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| Online Access: | https://journal.geo.sav.sk/cgg/article/view/9 |