Mineralogical investigation of degraded kaolinites from Dunántúl (Transdanubian) area
In the Dunántúl area clay occurrences with degraded kaolinite were found. These kaolinites can be well characterised by thermoanalytical methods. In the X-ray diffraction pattern the basal reflection is absent.
Elmentve itt :
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| Testületi szerző: | |
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1980
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| Sorozat: | Acta mineralogica-petrographica
24 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24678 |
| Tartalmi kivonat: | In the Dunántúl area clay occurrences with degraded kaolinite were found. These kaolinites can be well characterised by thermoanalytical methods. In the X-ray diffraction pattern the basal reflection is absent. |
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| Terjedelem/Fizikai jellemzők: | 111-114 |
| ISSN: | 0365-8066 |