Hydrothermal calcite veins and the origin of caves in the Lower Palaeozoic of the Barrandian Basin, Czech Republic: evidence of extensive (post?) Variscan fluid flow

SUCHÝ, V., ZEMAN, A., BOSÁK, P., DOBEŠ, P., HLADÍKOVÁ, J., JACKOVÁ, I. Hydrothermal calcite veins and the origin of caves in the Lower Palaeozoic of the Barrandian Basin, Czech Republic: evidence of extensive (post?) Variscan fluid flow. In: BECHSTÄDT, T., BENGTSON, P., GREILING, R., SCHWEIZER, V., eds. Abstracts. Gaea heidelbergensis. Heidelberg: Institute of Geology and Palaeontology, RuprechtKarlsUniversity, 1997, s. 325.