Origin of quartz veins near Velká Kraš in the Silesicum
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F10%3A00047098" target="_blank" >RIV/00216224:14310/10:00047098 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
čeština
Original language name
Geneze křemenných žil u Velké Kraše v sileziku
Original language 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). Basedon 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.
Czech name
Geneze křemenných žil u Velké Kraše v sileziku
Czech 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). Basedon 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.
Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geol. výzk. Mor. Slez.
ISSN
1212-6209
e-ISSN
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Volume of the periodical
17
Issue of the periodical within the volume
1-2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
3
Pages from-to
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UT code for WoS article
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EID of the result in the Scopus database
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