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

0145005 - GLU-S 20000001 RIV NL eng J - Článek v odborném periodiku
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
Grant CEP: GA AV ČR IAA3012703; GA AV ČR KSK1067601; GA AV ČR KSK1042603
Výzkumný záměr: CEZ:AV0Z3013912
Kód oboru RIV: DD - Geochemie
Impakt faktor: 1.182, rok: 2000

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.
Trvalý link: http://hdl.handle.net/11104/0042620