Fluid inclusion study of the Horní Luby cinnabar deposit, Saxothuringian Zone, Bohemian Massif: clues for the metamorphic remobilization of mercury
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10174052" target="_blank" >RIV/00216208:11310/13:10174052 - isvavai.cz</a>
Alternative codes found
RIV/00023272:_____/13:#0002124
Result on the web
<a href="http://dx.doi.org/10.3190/jgeosci.145" target="_blank" >http://dx.doi.org/10.3190/jgeosci.145</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3190/jgeosci.145" target="_blank" >10.3190/jgeosci.145</a>
Alternative languages
Result language
angličtina
Original language name
Fluid inclusion study of the Horní Luby cinnabar deposit, Saxothuringian Zone, Bohemian Massif: clues for the metamorphic remobilization of mercury
Original language description
The stratiform deposit of mercury at Horní Luby near Cheb (Czech Republic) is hosted by Ordovician phyllites of Vogtland-Saxony Paleozoic Unit in the Saxothuringian Zone of the Bohemian Massif. Ore is represented by cinnabar disseminated within the phyllite and by lenticular bodies rich in massive cinnabar (lenses with a thickness of up to 1 m and length along the strike varying from less than 1 m up to 20 m). Cinnabar is accompanied by pyrite and locally also siderite. The P-T history of the mineralization was deciphered by the study of fluid inclusions. Early fluids are fluid trapped in secretion quartz. This fluid underwent several heterogenization events starting from approximately 300 oC and continued down to 200-150 oC. Metamorphic quartz of secretion origin crystallized at ~300 oC, while hydrothermal pyrite crystallized at 220-210 oC and cinnabar at 195-160 oC. The formation of the richest ore was associated with the replacement of metamorphic quartz in phyllites by the cinnabar
Czech name
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Czech description
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Classification
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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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Geosciences
ISSN
1802-6222
e-ISSN
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Volume of the periodical
58
Issue of the periodical within the volume
3
Country of publishing house
CA - CANADA
Number of pages
16
Pages from-to
283-298
UT code for WoS article
000329990900008
EID of the result in the Scopus database
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