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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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    0145005 - GLU-S 20000001 RIV NL eng J - Journal Article
    Suchý, Václav - Heijlen, W. - Sýkorová, Ivana - Muchez, Ph. - Dobeš, P. - Hladíková, J. - Jačková, I. - Šafanda, Jan - Zeman, Antonín
    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.
    Sedimentary geology. Roč. 131, 3/4 (2000), s. 201-219. ISSN 0037-0738. E-ISSN 1879-0968
    R&D Projects: GA AV ČR IAA3012703; GA AV ČR KSK1067601; GA AV ČR KSK1042603
    Institutional research plan: CEZ:AV0Z3013912
    Subject RIV: DD - Geochemistry
    Impact factor: 1.182, year: 2000
    DOI: https://doi.org/10.1016/S0037-0738(99)00136-0

    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.
    Permanent Link: http://hdl.handle.net/11104/0042620
     

Number of the records: 1  

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