About: Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm     Goto   Sponge   NotDistinct   Permalink

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Description
  • Hydrothermal mineralizations of Variscan and Post-Variscan ages with high proportion of carbonates (calcite, dolomite-ankerite, siderite) are widespread in the Moravo-Silesian Culm formations at the north-eastern margin of the Bohemian Massif. Results of a detailed study (chemistry, isotopic composition, fluid inclusions) of vein carbonates are presented in this work. Older Variscan epithermal (to mesothermal ?)syntectonic mineralization is represented by quartz-calcite veins with clinochlore-chamosite chlorite, rare pyrite. Younger hydrothermal mineralization is formed mainly by carbonates and quartz. Sulphides are represented by galena, sphalerite, chalcopyrite, pyrite and locally marcasite. Boht types of mineralization often occur in one vein.
  • Hydrothermal mineralizations of Variscan and Post-Variscan ages with high proportion of carbonates (calcite, dolomite-ankerite, siderite) are widespread in the Moravo-Silesian Culm formations at the north-eastern margin of the Bohemian Massif. Results of a detailed study (chemistry, isotopic composition, fluid inclusions) of vein carbonates are presented in this work. Older Variscan epithermal (to mesothermal ?)syntectonic mineralization is represented by quartz-calcite veins with clinochlore-chamosite chlorite, rare pyrite. Younger hydrothermal mineralization is formed mainly by carbonates and quartz. Sulphides are represented by galena, sphalerite, chalcopyrite, pyrite and locally marcasite. Boht types of mineralization often occur in one vein. (en)
  • Hydrothermal mineralizations of Variscan and Post-Variscan ages with high proportion of carbonates (calcite, dolomite-ankerite, siderite) are widespread in the Moravo-Silesian Culm formations at the north-eastern margin of the Bohemian Massif. Results of a detailed study (chemistry, isotopic composition, fluid inclusions) of vein carbonates are presented in this work. Older Variscan epithermal (to mesothermal ?)syntectonic mineralization is represented by quartz-calcite veins with clinochlore-chamosite chlorite, rare pyrite. Younger hydrothermal mineralization is formed mainly by carbonates and quartz. Sulphides are represented by galena, sphalerite, chalcopyrite, pyrite and locally marcasite. Boht types of mineralization often occur in one vein. (cs)
Title
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm (en)
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm (cs)
skos:prefLabel
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm (en)
  • Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm (cs)
skos:notation
  • RIV/00216224:14310/03:00008898!RIV08-MSM-14310___
http://linked.open.../vavai/riv/strany
  • 111-122
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM 143100004), Z(MZP:N03/98:00)
http://linked.open...iv/cisloPeriodika
  • 3-4
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
  • 629623
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/03:00008898
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Moravo-Silesian Culm; hydrothermal mineralization; carbonates; chemistry; carbon isotopes; oxygen isotopes; fluid inclusions (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [18991B7FA6F4]
http://linked.open...i/riv/nazevZdroje
  • Journal of the Czech Geol. Soc.
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 47
http://linked.open...iv/tvurceVysledku
  • Losos, Zdeněk
  • Novotný, Pavel
  • Zimák, Jiří
  • Dobeš, Petr
  • Hladíková, Jana
http://linked.open...n/vavai/riv/zamer
issn
  • 1210-8197
number of pages
http://localhost/t...ganizacniJednotka
  • 14310
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