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Description
  • Fluid inclusions from the vein quartz near Velká Kraš 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.
  • Fluid inclusions from the vein quartz near Velká Kraš 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)
  • Fluid inclusions from the vein quartz near Velká Kraš 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)
Title
  • Geneze křemenných žil u Velké Kraše v sileziku
  • Origin of quartz veins near Velká Kraš in the Silesicum (en)
  • Geneze křemenných žil u Velké Kraše v sileziku (cs)
skos:prefLabel
  • Geneze křemenných žil u Velké Kraše v sileziku
  • Origin of quartz veins near Velká Kraš in the Silesicum (en)
  • Geneze křemenných žil u Velké Kraše v sileziku (cs)
skos:notation
  • RIV/00216224:14310/10:00047098!RIV11-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM0021622412), Z(MSM0021622427)
http://linked.open...iv/cisloPeriodika
  • 1-2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 260455
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/10:00047098
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Silesicum; quartz; fluid inclusions; oxygen isotopes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [07D782DFB101]
http://linked.open...i/riv/nazevZdroje
  • Geol. výzk. Mor. Slez.
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 17
http://linked.open...iv/tvurceVysledku
  • Přichystal, Antonín
  • Slobodník, Marek
  • Morávek, Rostislav
http://linked.open...n/vavai/riv/zamer
issn
  • 1212-6209
number of pages
http://localhost/t...ganizacniJednotka
  • 14310
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