Mineralogy and geochemistry of the lead-zinc mineralization at Ranga, Red Sea Coast
The mineral association of Ranga lead-zinc deposit is microscopically described. The trace elements assemblage in cubic and zonal galena is quantitatively determined. Besides, the trace elements in other minerals associated with galena were semiquantitatively estimated. The deposit is attributed to...
Elmentve itt :
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Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1982
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Sorozat: | Acta mineralogica-petrographica
25 No. 2 |
Kulcsszavak: | Geokémia, Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24703 |
Tartalmi kivonat: | The mineral association of Ranga lead-zinc deposit is microscopically described. The trace elements assemblage in cubic and zonal galena is quantitatively determined. Besides, the trace elements in other minerals associated with galena were semiquantitatively estimated. The deposit is attributed to the exhalative sedimentary processes by which other Egyptian Miocene lead-zinc ores were similarly formed. |
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Terjedelem/Fizikai jellemzők: | 211-221 |
ISSN: | 0365-8066 |