. "Geneze k\u0159emenn\u00FDch \u017Eil u Velk\u00E9 Kra\u0161e v sileziku"@cs . "Slobodn\u00EDk, Marek" . . "Mor\u00E1vek, Rostislav" . "17" . "RIV/00216224:14310/10:00047098!RIV11-MSM-14310___" . . "3"^^ . . "[07D782DFB101]" . . "Geneze k\u0159emenn\u00FDch \u017Eil u Velk\u00E9 Kra\u0161e v sileziku"@cs . . . . "1212-6209" . . "260455" . "Z(MSM0021622412), Z(MSM0021622427)" . "CZ - \u010Cesk\u00E1 republika" . . . "Origin of quartz veins near Velk\u00E1 Kra\u0161 in the Silesicum"@en . "Fluid inclusions from the vein quartz near Velk\u00E1 Kra\u0161 have been investigated. Inclusions with two immiscible liquids, aqueous (L1) and carbonic (L2) one, have been found so far. Most of inclusions have a stable ratio of both liquids (L2/L1 = 0,1). Based on petrographic observation we could state that fluids might be trapped close to the one phase and two phase boundary of the H2O-NaCl-CO2 system. The two cogenetic fluid inclusions, with immiscible CO2-rich and H2O-rich fluid phases, have been used for an estimation of the p-T conditions. The temperature 320 degC and presure 2050 bars could be a lower limit for the precipitation of the quartz. The salinity of the aqueous solution is 4,5 mass% NaCl eq. The trapped fluids show a nature of the pegmatite post-magmatic solutions."@cs . . "Silesicum; quartz; fluid inclusions; oxygen isotopes"@en . "RIV/00216224:14310/10:00047098" . . "1"^^ . "Fluid inclusions from the vein quartz near Velk\u00E1 Kra\u0161 have been investigated. Inclusions with two immiscible liquids, aqueous (L1) and carbonic (L2) one, have been found so far. Most of inclusions have a stable ratio of both liquids (L2/L1 = 0,1). Based on petrographic observation we could state that fluids might be trapped close to the one phase and two phase boundary of the H2O-NaCl-CO2 system. The two cogenetic fluid inclusions, with immiscible CO2-rich and H2O-rich fluid phases, have been used for an estimation of the p-T conditions. The temperature 320 degC and presure 2050 bars could be a lower limit for the precipitation of the quartz. The salinity of the aqueous solution is 4,5 mass% NaCl eq. The trapped fluids show a nature of the pegmatite post-magmatic solutions."@en . "Geneze k\u0159emenn\u00FDch \u017Eil u Velk\u00E9 Kra\u0161e v sileziku" . "14310" . "P\u0159ichystal, Anton\u00EDn" . . "1-2" . "3"^^ . . "Geol. v\u00FDzk. Mor. Slez." . "Fluid inclusions from the vein quartz near Velk\u00E1 Kra\u0161 have been investigated. Inclusions with two immiscible liquids, aqueous (L1) and carbonic (L2) one, have been found so far. Most of inclusions have a stable ratio of both liquids (L2/L1 = 0,1). Based on petrographic observation we could state that fluids might be trapped close to the one phase and two phase boundary of the H2O-NaCl-CO2 system. The two cogenetic fluid inclusions, with immiscible CO2-rich and H2O-rich fluid phases, have been used for an estimation of the p-T conditions. The temperature 320 degC and presure 2050 bars could be a lower limit for the precipitation of the quartz. The salinity of the aqueous solution is 4,5 mass% NaCl eq. The trapped fluids show a nature of the pegmatite post-magmatic solutions." . . "Geneze k\u0159emenn\u00FDch \u017Eil u Velk\u00E9 Kra\u0161e v sileziku" . . "Origin of quartz veins near Velk\u00E1 Kra\u0161 in the Silesicum"@en .