KUČERA, Jan, Jan CEMPÍREK, Zdeněk DOLNÍČEK, Philippe MUCHEZ and Walter PROCHASKA. Rare earth elements and yttrium geochemistry of dolomite from post-Variscan vein-type mineralization of the Nízký Jeseník and Upper Silesian Basins, Czech Republic. Journal of Geochemical Exploration. Nizozemské království: Elsevier, 2009, vol. 103, 2-3, p. 69-79. ISSN 0375-6742.
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Basic information
Original name Rare earth elements and yttrium geochemistry of dolomite from post-Variscan vein-type mineralization of the Nízký Jeseník and Upper Silesian Basins, Czech Republic
Name in Czech Geochemie REE a Y dolomitu z post-Variské žilné mineralizace Nízkého Jeseníku a hornoslezské pánve, Česká Republika
Authors KUČERA, Jan, Jan CEMPÍREK, Zdeněk DOLNÍČEK, Philippe MUCHEZ and Walter PROCHASKA.
Edition Journal of Geochemical Exploration, Nizozemské království, Elsevier, 2009, 0375-6742.
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 Netherlands
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.791
Organization unit Faculty of Science
UT WoS 000271542100002
Keywords (in Czech) Český masiv, prvky vzácných zemin, ytrium, dolomit, hydrotermální žíly, post-Variská fluida
Keywords in English Bohemian Massif, Rare earth elements, Yttrium, Dolomite, Hydrothermal veins, Post-Variscan fluid flow
Tags International impact, Reviewed
Changed by Changed by: doc. Mgr. Jan Cempírek, Ph.D., učo 15719. Changed: 25/8/2015 14:47.
Abstract
Rare earth elements and yttrium geochemistry of dolomite from post-Variscan vein-type Zn–Pb–Cu mineralization was studied in the Nízký Jeseník and Upper Silesian Basins. Combined with crush–leach analyses of fluid inclusions, the study provided important information on fluid–rock interaction, physicochemical and redox conditions during crystallization of the dolomite.
Abstract (in Czech)
Geochemie REE a Y dolomitu z post-Variských žilných Zn–Pb–Cu mineralizací byla studována v Nízkém Jeseníku a hornoslezské pánvi. V kombinaci s crush–leach analýzami fluidních inkluzí, studium poskytlo podstatné informace o interakci fluida–hornina a o fyzikálně-chemických podmínkách během krystalizace dolomitu.
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