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Hakite from Příbram, Czech Republic: compositional variability, crystal structure and the role in Se mineralization
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SYSNO ASEP 0467741 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Hakite from Příbram, Czech Republic: compositional variability, crystal structure and the role in Se mineralization Author(s) Škácha, P. (CZ)
Sejkora, J. (CZ)
Palatinus, Lukáš (FZU-D) RID, ORCID
Makovicky, E. (DK)
Plášil, Jakub (FZU-D) RID, ORCID
Macek, I. (CZ)
Goliáš, V. (CZ)Source Title Mineralogical Magazine - ISSN 0026-461X
Roč. 80, č. 6 (2016), s. 1115-1128Number of pages 14 s. Language eng - English Country GB - United Kingdom Keywords hakite ; selenides ; tetrahedrite group ; crystal structure ; Příbram ; uranium district ; analyses ; diffraction data Subject RIV DB - Geology ; Mineralogy Institutional support FZU-D - RVO:68378271 UT WOS 000391201100016 EID SCOPUS 84999287150 DOI 10.1180/minmag.2016.080.038 Annotation Hakite, ideally Cu10Hg2Sb4Se13 , is a Se-dominant member of the tetrahedrite group occurring at only a few
localities in theWorld. A new occurrence of this mineral in the Příbram 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.Workplace Institute of Physics Contact Kristina Potocká, potocka@fzu.cz, Tel.: 220 318 579 Year of Publishing 2017
Number of the records: 1