Publication details

The variability of chemical composition of the syntectonic fluids, Moravo-Silesian Paleozoic

Authors

POŘÁDEK Přemysl SLOBODNÍK Marek

Year of publication 2015
Type Conference abstract
MU Faculty or unit

Faculty of Science

Citation
Description Hydrothermal syntectonic veins are widespread throughout sedimentary sequences of Moravo-Silesian Paleozoic. This veins are mainly made up of quartz, calcite and chlorite. Four localities are in centre of our interest. There are 2 types of fluid inclusions in quartz (primary and pseudosecondary) which were investigated – liquid (L) + vapor (V) and vapor only. Chemical composition of L+V inclusion were determined as H2O-NaCl ± Mg, K, and Fe chloride, meanwhile chemical compostition of vapour-rich inclusion is CH4-CO2. Homogenization temperatures of two-phase inclusions vary between 112 to 348°C. The ice-melting temperatures suggest low salinity of fluids. Methane is dominating species in CH4-CO2 inclusions. Chlorite geothermometry were applied only on samples from western part of the area. These temparatures correspond to the temperatures obtained from microthermometry.

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