Data on the dickite occurrence of Mád (Hungary)

Mezősi József: Data on the dickite occurrence of Mád (Hungary). In: Acta mineralogica-petrographica, (10). pp. 67-75. (1957)

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Abstract

The rhyolite tuffs of the Sarmatian age in the surroundings of Mád were kaolinized on the action of hydrothermal fluids. The smaller and larger hollows of the porous tuff is filled out with dickite and kaolinite. The dickite could be identified by DTA as well as X-ray pattern. Dickite appears as 15—20 l1 long and 3—8 wide crystals and the kaolinite always in dense aggregations of micron sized .granules. The fact that it is associated with kaolinite shows that special conditions are necessary for it to form, these are, however, still fairly unexplored.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1957
Volume: 10
ISSN: 0365-8066
Page Range: pp. 67-75
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39376/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 74-75. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:27
Last Modified: 2022. Jul. 21. 09:10
URI: http://acta.bibl.u-szeged.hu/id/eprint/24430

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