ZIMÁK, Jiří, Zdeněk LOSOS, Pavel NOVOTNÝ, Petr DOBEŠ and Jana HLADÍKOVÁ. Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm. Journal of the Czech Geol. Soc. Praha: Czech Geol. Soc., vol. 47, 3-4, p. 111-122. ISSN 1210-8197. 2003.
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Basic information
Original name Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
Authors ZIMÁK, Jiří (203 Czech Republic), Zdeněk LOSOS (203 Czech Republic, guarantor), Pavel NOVOTNÝ (203 Czech Republic), Petr DOBEŠ (203 Czech Republic) and Jana HLADÍKOVÁ (203 Czech Republic).
Edition Journal of the Czech Geol. Soc. Praha, Czech Geol. Soc. 2003, 1210-8197.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Czech Republic
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/03:00008898
Organization unit Faculty of Science
Keywords in English Moravo-Silesian Culm; hydrothermal mineralization; carbonates; chemistry; carbon isotopes; oxygen isotopes; fluid inclusions
Tags carbon isotopes, carbonates, chemistry, fluid inclusions, hydrothermal mineralization, Moravo-Silesian Culm, oxygen isotopes
Changed by Changed by: doc. RNDr. Zdeněk Losos, CSc., učo 2470. Changed: 3/10/2003 13:11.
Abstract
Hydrothermal mineralizations of Variscan and Post-Variscan ages with high proportion of carbonates (calcite, dolomite-ankerite, siderite) are widespread in the Moravo-Silesian Culm formations at the north-eastern margin of the Bohemian Massif. Results of a detailed study (chemistry, isotopic composition, fluid inclusions) of vein carbonates are presented in this work. Older Variscan epithermal (to mesothermal ?)syntectonic mineralization is represented by quartz-calcite veins with clinochlore-chamosite chlorite, rare pyrite. Younger hydrothermal mineralization is formed mainly by carbonates and quartz. Sulphides are represented by galena, sphalerite, chalcopyrite, pyrite and locally marcasite. Boht types of mineralization often occur in one vein.
Links
MSM 143100004, plan (intention)Name: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid
Investor: Ministry of Education, Youth and Sports of the CR, Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides
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