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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F10%3A00047098%21RIV11-MSM-14310___
rdf:type
n7:Vysledek skos:Concept
dcterms: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. 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.
dcterms:title
Geneze křemenných žil u Velké Kraše v sileziku Origin of quartz veins near Velká Kraš in the Silesicum Geneze křemenných žil u Velké Kraše v sileziku
skos:prefLabel
Geneze křemenných žil u Velké Kraše v sileziku Geneze křemenných žil u Velké Kraše v sileziku Origin of quartz veins near Velká Kraš in the Silesicum
skos:notation
RIV/00216224:14310/10:00047098!RIV11-MSM-14310___
n3:aktivita
n9:Z
n3:aktivity
Z(MSM0021622412), Z(MSM0021622427)
n3:cisloPeriodika
1-2
n3:dodaniDat
n17:2011
n3:domaciTvurceVysledku
n15:5910250
n3:druhVysledku
n14:J
n3:duvernostUdaju
n6:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
260455
n3:idVysledku
RIV/00216224:14310/10:00047098
n3:jazykVysledku
n18:cze
n3:klicovaSlova
Silesicum; quartz; fluid inclusions; oxygen isotopes
n3:klicoveSlovo
n10:oxygen%20isotopes n10:fluid%20inclusions n10:quartz n10:Silesicum
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[07D782DFB101]
n3:nazevZdroje
Geol. výzk. Mor. Slez.
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n17:2010
n3:svazekPeriodika
17
n3:tvurceVysledku
Slobodník, Marek Morávek, Rostislav Přichystal, Antonín
n3:zamer
n4:MSM0021622412 n4:MSM0021622427
s:issn
1212-6209
s:numberOfPages
3
n16:organizacniJednotka
14310