Characterization of kaolin minerals of different origin (essentially from Hungarian deposits) /
Kaolinite minerals from weathered rhyolite tuff's, from sedimentary kaolin clays, bauxites and argillaceous lignites were studied by X-ray diffractographic, infrared-spectroscopic and thermoanalytic methods. In addition to determining the mineralogical composition and the grain size distributio...
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/24676 |
| LEADER | 01844nab a2200241 i 4500 | ||
|---|---|---|---|
| 001 | acta24676 | ||
| 005 | 20220725132815.0 | ||
| 008 | 161017s1980 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Kocsárdy Éva | |
| 245 | 1 | 0 | |a Characterization of kaolin minerals of different origin |h [elektronikus dokumentum] : |b (essentially from Hungarian deposits) / |c Kocsárdy Éva |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1980 | ||
| 300 | |a 91-99 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 24 | |
| 520 | 3 | |a Kaolinite minerals from weathered rhyolite tuff's, from sedimentary kaolin clays, bauxites and argillaceous lignites were studied by X-ray diffractographic, infrared-spectroscopic and thermoanalytic methods. In addition to determining the mineralogical composition and the grain size distribution of bulk samples, the authors obtained closer characterization of various kaolinite minerals by measuring the polytypes and the crystallinity state of the minerals. X-ray diffractography was used for assessing the Hinkley index and the half-width of the 001-reflection, while infrared techniques were resorted to for assessing, among other things, the Kt-index (Kt = E3M5 cm ~ ' / E3620 cm- 1 ) and the K2-index (K2=E3670+E365 0 + E3620/E3695). All these results should be relied on for attempting to distinguish between kaolinites of different genesis. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 700 | 0 | 1 | |a Heydemann Annerose |e aut |
| 710 | |a International Kaolin Symposium (10.) (1979) (Budapest) | ||
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24676/1/mineralogica_024_suppl_091-099.pdf |z Dokumentum-elérés |