S,F,Cl -Rich mineral assemblages from burned spoil heaps in the Rosice-Oslavany coalfield, Czech Republic

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F13%3A33144457" target="_blank" >RIV/61989592:15310/13:33144457 - isvavai.cz</a>
Alternative codes found
RIV/00094862:_____/13:#0001588 RIV/00023272:_____/13:#0002120
Result on the web
<a href="http://dx.doi.org/10.3749/canmin.51.1.171" target="_blank" >http://dx.doi.org/10.3749/canmin.51.1.171</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3749/canmin.51.1.171" target="_blank" >10.3749/canmin.51.1.171</a>

Result language
angličtina
Original language name
S,F,Cl -Rich mineral assemblages from burned spoil heaps in the Rosice-Oslavany coalfield, Czech Republic
Original language description
Rare oxide-sulfosilicate-sulfate mineral assemblages have been identified in burned material from two spoil heaps (Kukla mine, Oslavany, and Ferdinand mine, Zastávka) in the Rosice-Oslavany coalfield, Czech Republic. The assemblages are deficient in Si and Al, and contain high amounts of fluorine and chlorine; major minerals are gypsum, anhydrite, fluorellestadite, periclase, brucite, and portlandite. Accessory minerals include magnesioferrite, Mn-rich srebrodolskite, and rare kumtyubeite, Fe,Cl-rich brearleyite/mayenite, wadalite, fluorite, cuspidine, rondorfite, and an unnamed mineral with composition Ca4(Mn,Fe)2O7. The assemblages are pyrometamorphic products of a dolomite-anhydrite-gypsum protolith, at Tmin } 800°C. The most probable source of halogens was organic matter.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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