Detailed Information on Publication Record
2006
Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Rožná uranium deposit, Western Moravia, Czech Republic
DOLEŽALOVÁ, Hana, Stanislav HOUZAR, Zdeněk LOSOS and Radek ŠKODABasic information
Original name
Kinoshitalite with a high magnesium content in sulphide-rich marbles from the Rožná uranium deposit, Western Moravia, Czech Republic
Name in Czech
Vysoce hořečnatý kinoshitalit v mramorech bohatých sulfidy z uranového ložiska Rožná, Západní Morava, Česká Republika
Authors
DOLEŽALOVÁ, Hana (203 Czech Republic), Stanislav HOUZAR (203 Czech Republic), Zdeněk LOSOS (203 Czech Republic, guarantor) and Radek ŠKODA (203 Czech Republic)
Edition
Neues Jahrbuch fur Mineralogie, Abhandlungen, Stuttgart, E.Schweitzerbatsch Verlagsbuchhandlung, 2006, 0028-3649
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Germany
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 0.487
RIV identification code
RIV/00216224:14310/06:00016622
Organization unit
Faculty of Science
UT WoS
000237799600005
Keywords in English
kinoshitalite; Ba-micas; sphalerite; marble; Rožná uranium deposit; Moldanubicum; Bohemian Massif; Czech Republic
Tags
Změněno: 26/4/2006 12:14, doc. RNDr. Zdeněk Losos, CSc.
V originále
Ba-micas including magnesian kinoshitalite (XMg more than 0.99) were found in sulphide-rich dolomite marbles at the Rožná uranium deposit, Moldanubicum, Czech Republic. The Ba-micas (phlogopite with Ba > 0.280 apfu and kinoshitalite with Ba from 0.869 to 1.244 apfu) are Mn, Fe and Ti-poor in comparison to other Ba-micas described up to date. The main substitution mechanism in Ba-micas is (Ba2+,Ca2+) (Al3+) (K+,Na+)-1 Si4+-1. Relatively high content of Mn in silicates and carbonates from the host marble is in contrast to the chemistry of Ba-micas. Barium and manganese show distinct behaviour during metamorphism. Manganese and iron were probably partitioned to metamorphic sphalerite and pyrrhotite relative to (Mn, Fe)-poor Ba-micas. Barium concentrated in mica minerals and the system was evidently Ba-depleted in late stages.
In Czech
Ba-slídy včetně Mg-bohatého kinoshitalitu, byly nalezeny v dolomitických mramorech s vtroušenými sulfidy v prostoru uranového ložiska Rožná, moldanubikum, Česká republika. Uvedené fylosilikáty jsou podrobně mineralogicky popsány a analyzovány, řešeny jsou migrace a redistribuce Ba, Mn a Fe mezi metamorfními minerály a sulfidy mramorů.
Links
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