A classification for sedimentary kaolinitic formations of economic importance
A wide range of sedimentary geological formations of which kaolin is a major constituent are used industrially for a wide range of uses, ranging from paper to ceramics. All these formations are of fresh water origin and can be looked at as a continuous series ranging from ball clays with high streng...
Elmentve itt :
Szerző: | |
---|---|
Testületi szerző: | |
Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1980
|
Sorozat: | Acta mineralogica-petrographica
24 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24668 |
LEADER | 01489nab a2200229 i 4500 | ||
---|---|---|---|
001 | acta24668 | ||
005 | 20220725125143.0 | ||
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 Bristow C. M. | |
245 | 1 | 2 | |a A classification for sedimentary kaolinitic formations of economic importance |h [elektronikus dokumentum] / |c Bristow C. M. |
260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1980 | ||
300 | |a 19-25 | ||
490 | 0 | |a Acta mineralogica-petrographica |v 24 | |
520 | 3 | |a A wide range of sedimentary geological formations of which kaolin is a major constituent are used industrially for a wide range of uses, ranging from paper to ceramics. All these formations are of fresh water origin and can be looked at as a continuous series ranging from ball clays with high strength and plasticity at one end of the series to sedimentary kaolins with good powder brightness and rheology at the other end. The changes in commercial characteristics from one end of the series to the other can be related to the mineralogy of the sediments. | |
650 | 4 | |a Természettudományok | |
650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
695 | |a Kőzettan, Ásványtan, Földtan | ||
710 | |a International Kaolin Symposium (10.) (1979) (Budapest) | ||
856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24668/1/mineralogica_024_suppl_019-025.pdf |z Dokumentum-elérés |