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Geochemical study of calcite veins in the Silurian and Devonian of the Barrandian Basin (Czech Republic): evidence for widespread post-Variscan fluid flow in the central part of the Bohemian Massif
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SYSNO ASEP 0145005 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Geochemical study of calcite veins in the Silurian and Devonian of the Barrandian Basin (Czech Republic): evidence for widespread post-Variscan fluid flow in the central part of the Bohemian Massif Author(s) Suchý, Václav (GLU-S) SAI
Heijlen, W. (NL)
Sýkorová, Ivana (USMH-B) RID, ORCID
Muchez, Ph. (NL)
Dobeš, P. (CZ)
Hladíková, J. (CZ)
Jačková, I. (CZ)
Šafanda, Jan (GFU-E) ORCID, RID
Zeman, Antonín (GLU-S)Source Title Sedimentary geology. - : Elsevier - ISSN 0037-0738
Roč. 131, 3/4 (2000), s. 201-219Number of pages 19 s. Language eng - English Country NL - Netherlands Subject RIV DD - Geochemistry R&D Projects IAA3012703 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) KSK1067601 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) KSK1042603 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z3013912 - GLU-S UT WOS 000086129100008 EID SCOPUS 0034653252 DOI https://doi.org/10.1016/S0037-0738(99)00136-0 Annotation N-S-striking calcite veins that occur in lower Paleozoic sequences of the Barrandian basin (Czech Republic) precipitated from low-salinity fluid at temperatures ( 70°C. The veins probably reflect episodes of lineament-controlled fluid migration that occurred during late stages of the Variscan orogeny. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Tel.: 226 800 273 Year of Publishing 2001
Number of the records: 1