Correlation of mineral composition of the parent rock with the mineral composition of kaolin

Petrov V. P. and Samotoin N. D. and Fin'ko V. I. and Chekin S. S.: Correlation of mineral composition of the parent rock with the mineral composition of kaolin. In: Acta mineralogica-petrographica, (24). pp. 77-82. (1980)

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Abstract

Commercial kaolin deposits are only formed from acid rock. In the weathering processes quartz grains of primary rock are conserved without any changes of size. Large kaolinite flakes arise in the place of mica by epitaxial growth on a mica sheet. Some part of iron and titanium is preserved in special minerals formed within pseudomorphs after biotite. K-feldspar changes into small newly formed kaolinite flakes. On acid plagioclase halloysite appears but on andesine-labrador montmorillonite arises. Properties of commercial kaolin depend upon all the peculiarities of the mineral transformations.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1980
Volume: 24
ISSN: 0365-8066
Page Range: pp. 77-82
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Event Title: International Kaolin Symposium (10.) (1979) (Budapest)
Related URLs: http://acta.bibl.u-szeged.hu/39400/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 81-82. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:25
Last Modified: 2022. Jul. 25. 14:45
URI: http://acta.bibl.u-szeged.hu/id/eprint/24674

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