KUČERA, Jan, Klára KUČEROVÁ CHARVÁTOVÁ, Phillipe MUCHEZ and Walter PROCHASKA. Palaeofluid flow in siliciclastic Lower Carboniferous rocks: Evidence from stable isotopes and fluid inclusions, Rhenohercynian Zone, Czech Republic. In Mineral Deposit Research: Meeting the Global Challenge. Berlín: Springer-Verlag, 2005, p. 137-139, 871 s. ISBN 3-540-27945-8. |
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@inproceedings{579381, author = {Kučera, Jan and Kučerová Charvátová, Klára and Muchez, Phillipe and Prochaska, Walter}, address = {Berlín}, booktitle = {Mineral Deposit Research: Meeting the Global Challenge}, keywords = {Bohemian Massif; dolomite; stable isotopes; fluid inclusions; crush-leach analyses}, location = {Berlín}, isbn = {3-540-27945-8}, pages = {137-139}, publisher = {Springer-Verlag}, title = {Palaeofluid flow in siliciclastic Lower Carboniferous rocks: Evidence from stable isotopes and fluid inclusions, Rhenohercynian Zone, Czech Republic.}, year = {2005} }
TY - JOUR ID - 579381 AU - Kučera, Jan - Kučerová Charvátová, Klára - Muchez, Phillipe - Prochaska, Walter PY - 2005 TI - Palaeofluid flow in siliciclastic Lower Carboniferous rocks: Evidence from stable isotopes and fluid inclusions, Rhenohercynian Zone, Czech Republic. PB - Springer-Verlag CY - Berlín SN - 3540279458 KW - Bohemian Massif KW - dolomite KW - stable isotopes KW - fluid inclusions KW - crush-leach analyses N2 - Post-Variscan Zn, Pb, Cu vein mineralisation occurs within the Lower Carboniferous siliciclastic rocks at the eastern border of the Bohemian Massif. Saddle dolomites are associated with this vein mineralisation and indicate a NW-SE oriented fluid flow through the Palaeozoic rocks. The major control on this fluid flow pattern is exerted by the faults. Eutectic temperature and crush-leach analyses indicate H2O-NaCl-CaCl2 type of basinal brines. Homogenization temperatures regionally decrease from 147 to 80C and salinities from 26.5 to 17 wt.% eq.NaCl. Temperatures correlate well with an increase of d18O values from 15.5 to 22.5 SMOW and d13C values from -5.6 to -3.1 PDB. ER -
KUČERA, Jan, Klára KUČEROVÁ CHARVÁTOVÁ, Phillipe MUCHEZ and Walter PROCHASKA. Palaeofluid flow in siliciclastic Lower Carboniferous rocks: Evidence from stable isotopes and fluid inclusions, Rhenohercynian Zone, Czech Republic. In \textit{Mineral Deposit Research: Meeting the Global Challenge}. Berlín: Springer-Verlag, 2005, p.~137-139, 871 s. ISBN~3-540-27945-8.
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