Mg-minerals of recent hydrothermal formations of the Cu-porphyric mineralisation at Recsk, Hungary
A great variety of minerals precipitated from thermal waters (35—44 °C) were observed in the drifts of the copper-porphyritic skarn ore deposit at Recsk. Beside calcite-aragonite and various salts with different solubility, the Mg-minerals (nesquehonite—dypingite—hydromagnesite—giorgiositenorthupite...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1993
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| Sorozat: | Acta mineralogica-petrographica
34 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24806 |
| LEADER | 02121nab a2200229 i 4500 | ||
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| 001 | acta24806 | ||
| 005 | 20220727102229.0 | ||
| 008 | 161017s1993 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Kiss János | |
| 245 | 1 | 0 | |a Mg-minerals of recent hydrothermal formations of the Cu-porphyric mineralisation at Recsk, Hungary |h [elektronikus dokumentum] / |c Kiss János |
| 260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1993 | ||
| 300 | |a 7-19 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 34 | |
| 520 | 3 | |a A great variety of minerals precipitated from thermal waters (35—44 °C) were observed in the drifts of the copper-porphyritic skarn ore deposit at Recsk. Beside calcite-aragonite and various salts with different solubility, the Mg-minerals (nesquehonite—dypingite—hydromagnesite—giorgiositenorthupite—astrakhanite— /vanthoffite; langbeinite/ —epsomite—palygorskite) have outstanding importance at this locality. The present work focussea on the study and interpretation of the hydrothermal formation of the Mg-minerals otherwise known as hypergenitic evaporites. AUSZUG : In den Stollen des porohyrischen-skarn Cu-Erzlagers in Recsk ist eine ausserordentlich grosse Variation von hydrothermalen (35—44 °C) Mineralienabsonderungen vorhanden. Unter den KalzitAragonit-, und anderen Mineralsalzen von veränderlicher Lösbarkeit spielen die Magnesiumminerale (Nesquehonit—Dypingit—Hydromagnesit—Giorgiosit—Northupit—Astrakhanit— /Vanthoffit; Langbeinit/— Epsomit—Palygorskit) eine beachtliche Rolle. In dieser Arbeit wird die hydrothermale Entstehung dieser, von anderen Lokalitäten meistens als hypergen-evaporitischen Phasen beschriebenen Mg-Mineralien untersucht und erklärt. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Kőzettan, Ásványtan, Földtan | ||
| 700 | 0 | 1 | |a Jánosi Melinda |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24806/1/mineralogica_034_007-019.pdf |z Dokumentum-elérés |