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Hakite from Pribram, Czech Republic: compositional variability, crystal structure and the role in Se mineralization

Publikace na Přírodovědecká fakulta |
2016

Tento text není v aktuálním jazyce dostupný. Zobrazuje se verze "en".Abstrakt

Hakite, ideally Cu10Hg2Sb4Se13, is a Se-dominant member of the tetrahedrite group occurring at only a few localities in the World. A new occurrence of this mineral in the Príbram uranium and base-metal ore district, Central Bohemia, Czech Republic, is reported in this paper.

Hakite was found to be locally abundant and was identified in several samples with Se mineralization. Three chemically distinct types of hakite were distinguished based on electron microprobe study, Hg-rich hakite (hakite sensu stricto), Zn-rich hakite and Cd-rich hakite.

Hg-hakite dominates among the samples studied.