Clay minerals from Asztagkő of Gyöngyössolymos

Mezősi József: Clay minerals from Asztagkő of Gyöngyössolymos. In: Acta mineralogica-petrographica, (10). pp. 59-66. (1957)

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Abstract

In the Asztagkő of Gyöngyössolymos at the boundary of the quartzite and the tuff there occurs, a colloidal substance which mostly consists of halioysite, limonite and hematite. The site of the exotherm peak appearing at 900—1000°C varies according to the amount of the iron content. The greater the amount of iron the lower the temperature at which the exotherm peak appears. The shift of the exotherm peak also takes place in the case of artificial mixtures.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1957
Volume: 10
ISSN: 0365-8066
Page Range: pp. 59-66
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. 65-66. ; 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. 09:07
URI: http://acta.bibl.u-szeged.hu/id/eprint/24429

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