Study of vein carbonates and notes to the genesis of the
hydrothermal mineralization in the Moravo-Silesian Culm

J 2003

Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm

ZIMÁK, Jiří, Zdeněk LOSOS, Pavel NOVOTNÝ, Petr DOBEŠ, Jana HLADÍKOVÁ et. al.

Základní údaje

Originální název

Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm

Autoři

ZIMÁK, Jiří (203 Česká republika), Zdeněk LOSOS (203 Česká republika, garant), Pavel NOVOTNÝ (203 Česká republika), Petr DOBEŠ (203 Česká republika) a Jana HLADÍKOVÁ (203 Česká republika)

Vydání

Journal of the Czech Geol. Soc. Praha, Czech Geol. Soc. 2003, 1210-8197

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/03:00008898

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Moravo-Silesian Culm; hydrothermal mineralization; carbonates; chemistry; carbon isotopes; oxygen isotopes; fluid inclusions

Štítky

carbon isotopes, carbonates, chemistry, fluid inclusions, hydrothermal mineralization, Moravo-Silesian Culm, oxygen isotopes

Změněno: 3. 10. 2003 13:11, doc. RNDr. Zdeněk Losos, CSc.

Anotace

V originále

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.

Návaznosti

MSM 143100004, záměr

Název: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Citovat

ZIMÁK, Jiří, Zdeněk LOSOS, Pavel NOVOTNÝ, Petr DOBEŠ a Jana HLADÍKOVÁ. Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm. Journal of the Czech Geol. Soc. Praha: Czech Geol. Soc., 2003, roč. 47, 3-4, s. 111-122. ISSN 1210-8197.

@article{488701,
   author = {Zimák, Jiří and Losos, Zdeněk and Novotný, Pavel and Dobeš, Petr and Hladíková, Jana},
   article_location = {Praha},
   article_number = {3-4},
   keywords = {Moravo-Silesian Culm; hydrothermal mineralization; carbonates; chemistry; carbon isotopes; oxygen isotopes; fluid inclusions},
   language = {eng},
   issn = {1210-8197},
   journal = {Journal of the Czech Geol. Soc.},
   title = {Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm},
   volume = {47},
   year = {2003}
}

TY  - JOUR
ID  - 488701
AU  - Zimák, Jiří - Losos, Zdeněk - Novotný, Pavel - Dobeš, Petr - Hladíková, Jana
PY  - 2003
TI  - Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm
JF  - Journal of the Czech Geol. Soc.
VL  - 47
IS  - 3-4
SP  - 111-122
EP  - 111-122
PB  - Czech Geol. Soc.
SN  - 12108197
KW  - Moravo-Silesian Culm
KW  - hydrothermal mineralization
KW  - carbonates
KW  - chemistry
KW  - carbon isotopes
KW  - oxygen isotopes
KW  - fluid inclusions
N2  - 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.
ER  -

ZIMÁK, Jiří, Zdeněk LOSOS, Pavel NOVOTNÝ, Petr DOBEŠ a Jana HLADÍKOVÁ. Study of vein carbonates and notes to the genesis of the hydrothermal mineralization in the Moravo-Silesian Culm. \textit{Journal of the Czech Geol. Soc.}. Praha: Czech Geol. Soc., 2003, roč.~47, 3-4, s.~111-122. ISSN~1210-8197.

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