Clay minerals from Asztagkő of Gyöngyössolymos
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 a...
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| Main Author: | |
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| Format: | Article |
| Published: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1957
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| Series: | Acta mineralogica-petrographica
10 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Subjects: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24429 |
| LEADER | 01296nab a2200217 i 4500 | ||
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| 008 | 161017s1957 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Mezősi József | |
| 245 | 1 | 0 | |a Clay minerals from Asztagkő of Gyöngyössolymos |h [elektronikus dokumentum] / |c Mezősi József |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1957 | ||
| 300 | |a 59-66 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 10 | |
| 520 | 3 | |a 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. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24429/1/mineralogica_010_059-066.pdf |z Dokumentum-elérés |