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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F03%3A00008898%21RIV08-MSM-14310___
rdf:type
skos:Concept n17:Vysledek
dcterms: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. 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.
dcterms: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 Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
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 Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
skos:notation
RIV/00216224:14310/03:00008898!RIV08-MSM-14310___
n3:strany
111-122
n3:aktivita
n13:Z
n3:aktivity
Z(MSM 143100004), Z(MZP:N03/98:00)
n3:cisloPeriodika
3-4
n3:dodaniDat
n6:2008
n3:domaciTvurceVysledku
n4:6218857 n4:3920143
n3:druhVysledku
n18:J
n3:duvernostUdaju
n7:S
n3:entitaPredkladatele
n8:predkladatel
n3:idSjednocenehoVysledku
629623
n3:idVysledku
RIV/00216224:14310/03:00008898
n3:jazykVysledku
n15:eng
n3:klicovaSlova
Moravo-Silesian Culm; hydrothermal mineralization; carbonates; chemistry; carbon isotopes; oxygen isotopes; fluid inclusions
n3:klicoveSlovo
n9:carbon%20isotopes n9:Moravo-Silesian%20Culm n9:hydrothermal%20mineralization n9:carbonates n9:chemistry n9:oxygen%20isotopes n9:fluid%20inclusions
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[18991B7FA6F4]
n3:nazevZdroje
Journal of the Czech Geol. Soc.
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
5
n3:rokUplatneniVysledku
n6:2003
n3:svazekPeriodika
47
n3:tvurceVysledku
Hladíková, Jana Losos, Zdeněk Novotný, Pavel Dobeš, Petr Zimák, Jiří
n3:zamer
n14:MZP%3AN03%2F98%3A00 n14:MSM%20143100004
s:issn
1210-8197
s:numberOfPages
12
n16:organizacniJednotka
14310