KUČEROVÁ CHARVÁTOVÁ, Klára, Jan KUČERA and Zdeněk DOLNÍČEK. Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian massif, Czech Republic. Berlin: Springer-Verlag. 1600 pp. 1. ISBN 3-540-27945-8. 2005.
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Basic information
Original name Origin and significance of calcite-marcasite-pyrite mineralisation in siliciclastic Lower Carboniferous rocks, eastern margin of the Bohemian massif, Czech Republic.
Name in Czech Původ a význam kalcit-markazit-pyritové mineralizace v siliciklastických horninách spodního karbonu na východním okraji Českého masivu, Česká republika.
Authors KUČEROVÁ CHARVÁTOVÁ, Klára, Jan KUČERA and Zdeněk DOLNÍČEK.
Edition Berlin, 1600 pp. 1, 2005.
Publisher Springer-Verlag
Other information
Original language English
Type of outcome Book on a specialized topic
Field of Study 10500 1.5. Earth and related environmental sciences
Confidentiality degree is not subject to a state or trade secret
Organization unit Faculty of Science
ISBN 3-540-27945-8
UT WoS 000237245800037
Keywords in English Bohemian Massif; calcite-marcasite mineralisation; stable isotopes; fluid inclusions
Tags Bohemian massif, calcite-marcasite mineralisation, fluid inclusions, Stable Isotopes
Changed by Changed by: Mgr. Klára Kučerová Charvátová, učo 55203. Changed: 23/9/2005 23:21.
Abstract
Field and petrographic observations combined with fluid inclusion measurements, geochemical data, and stable and radiogenic isotope results place important constraints on the genesis of calcite-marcasite-pyrite veinlets located in the Lower Carboniferous siliciclastic rocks of the Nízký Jeseník Upland. These data suggest that the veinlets formed from hydrothermal fluids derived from marine water that migrated, along with petroleum, out of the Carpathian Foredeep in Miocene time.
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