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@article{806471, author = {Kučera, Jan and Muchez, Philippe and Slobodník, Marek and Prochaska, Walter}, article_location = {Německo}, article_number = {99}, keywords = {Moravo-Silesian Palaeozoic; sedimentary sequences; dolomite veins; fluid chemistry; stable isotopes; water-rock interaction}, language = {eng}, issn = {1437-3262}, journal = {International Journal of Earth Sciences}, title = {Geochemistry of highly saline fluids in the Moravo-Silesian Palaeozoic siliciclastic sequences: genetic implications}, volume = {2010}, year = {2009} }
TY - JOUR ID - 806471 AU - Kučera, Jan - Muchez, Philippe - Slobodník, Marek - Prochaska, Walter PY - 2009 TI - Geochemistry of highly saline fluids in the Moravo-Silesian Palaeozoic siliciclastic sequences: genetic implications JF - International Journal of Earth Sciences VL - 2010 IS - 99 SP - 269-284 EP - 269-284 PB - Springer Berlin / Heidelberg SN - 14373262 KW - Moravo-Silesian Palaeozoic KW - sedimentary sequences KW - dolomite veins KW - fluid chemistry KW - stable isotopes KW - water-rock interaction N2 - Post-Variscan dolomites occur in Zn-Pb-Cu veins, Crush-leach, stable isotope (oxygen and carbon) and microthermometry analysis of the fluid inclusions in dolomites, Highly saline H2O-NaCl-CaCl2-MgCl2 fluids occur in inclusions, isotopic fluid composition indicate that the fluid was derived from evaporated seawater, rock-buffering explains the isotopic composition at low w/r ratios, fluid-rock interactions largely controlled the fluid chemistry (K, Li, Br and Na contents, K/Cl, I/Cl and Li/Cl molar ratios). A permeable basement and fractured sedimentary sequence enhanced the general nature of the fluid system. Fluid characteristics are comparable with the main post-Variscan fluid flow systems in the Polish (Cracow-Silesian ore district) and German sedimentary basins. ER -
KUČERA, Jan, Philippe MUCHEZ, Marek SLOBODNÍK a Walter PROCHASKA. Geochemistry of highly saline fluids in the Moravo-Silesian Palaeozoic siliciclastic sequences: genetic implications. Online. \textit{International Journal of Earth Sciences}. Německo: Springer Berlin / Heidelberg, 2009, roč.~2010, č.~99, s.~269-284, 25 s. ISSN~1437-3262. [citováno 2024-04-23]
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