SLOBODNÍK, Marek, Jiří ZIMÁK and Zdeněk DOLNÍČEK. Podmínky vzniku hydrotermální kalcit-křemen-sulfidické mineralizace u Hranic (Formation conditions of the calcite-quartz-sulphidic hydrothermal mineralization near Hranice). Geol. Výzk. Mor. Slez. v r. 2001. Brno: MU Brno, 2002, vol. 9, -, p. 62-64. ISSN 1212-6209.
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Basic information
Original name Podmínky vzniku hydrotermální kalcit-křemen-sulfidické mineralizace u Hranic
Name (in English) Formation conditions of the calcite-quartz-sulphidic hydrothermal mineralization near Hranice
Authors SLOBODNÍK, Marek (203 Czech Republic, guarantor), Jiří ZIMÁK (203 Czech Republic) and Zdeněk DOLNÍČEK (203 Czech Republic).
Edition Geol. Výzk. Mor. Slez. v r. 2001, Brno, MU Brno, 2002, 1212-6209.
Other information
Original language Czech
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/00216224:14310/02:00007216
Organization unit Faculty of Science
Keywords in English devonian limestones; calcite veins; stable isotopes; fluid inclusions; basinal brines
Tags basinal brines, calcite veins, Devonian limestones, fluid inclusions, Stable Isotopes
Tags International impact, Reviewed
Changed by Changed by: doc. RNDr. Marek Slobodník, CSc., učo 2488. Changed: 5/1/2009 13:35.
Abstract
Početné kalcitové žíly s křemenem a sulfidy proráží devonské vápence u Hranic. Jsou považovány za postvariskou mineralizaci. Vznikaly z nizkoteplotních (50-100C) fluid, které jsou odvozeny od pánevních solanek (typu H2O-NaCl-CaCl2).
Abstract (in English)
There are numerous calcite veins with quartz and little sulphides that cut through the Devonian limestones near Hranice. They are assumed to be a post-Variscan mineralization stage. Low temperature fluids (50 to 100C), from which hydrothermal minerals precipitated, can be best interpreted as mainly basinal brines (type H2O-NaCl-CaCl2).
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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