DOLNÍČEK, Zdenek and Marek SLOBODNÍK. The neoidic fluorite mineralization in the Brno massif: Interaction between fluid and rock. Geolines. Praha: AVČR, 2001, vol. 13, No 1, p. 51-52. ISSN 1210-9606.
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Basic information
Original name The neoidic fluorite mineralization in the Brno massif: Interaction between fluid and rock
Authors DOLNÍČEK, Zdenek and Marek SLOBODNÍK (203 Czech Republic, guarantor).
Edition Geolines, Praha, AVČR, 2001, 1210-9606.
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/00216224:14310/01:00004805
Organization unit Faculty of Science
Keywords in English fluorite; REE; fluid inclusions; stable isotopes
Tags fluid inclusions, fluorite, REE, Stable Isotopes
Tags International impact, Reviewed
Changed by Changed by: doc. RNDr. Marek Slobodník, CSc., učo 2488. Changed: 5/1/2009 13:45.
Abstract
Fluorite mineralization from granitoids of the Brno massif has been studied. Hydrothermal minerals precipitated from low saline fluids at temperatures of 80-150C and they were shallow-circulating meteoric waters. Mineralization could be compared with the Tertiary fluorite mineralization in the North Bohemia region (Teplice, Jílové u Děčína).
Abstract (in Czech)
Fluorite mineralization from granitoids of the Brno massif has been studied. Hydrothermal minerals precipitated from low saline fluids at temperatures of 80-150C and they were shallow-circulating meteoric waters. Mineralization could be compared with the Tertiary fluorite mineralization in the North Bohemia region (Teplice, Jílové u Děčína).
Links
GA205/00/0356, research and development projectName: Geochemický a tektonický model migrace fluid v paleozoiku moravskoslezské oblasti
Investor: Czech Science Foundation, Geochemical and tectonic model of fluid migration in the paleozoic of Moravo-Silesian region
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