DOLNÍČEK, Zdeněk, Tomáš LEHOTSKÝ, Marek SLOBODNÍK, Eva HEJTMÁNKOVÁ, Andrea GRÍGELOVÁ and Jan ZAPLETAL. Mineral-forming and diagenetic processes related to Tertiary hydrocarbon seepage at the Bohemian Massif/Outer Western Carpathians interface: Evidence from the Hrabůvka quarry, Moravia, Czech Republic. Marine and Petroleum Geology. Butterworth Scientific, 2014, vol. 52, April, p. 77-92. ISSN 0264-8172. Available from: https://dx.doi.org/10.1016/j.marpetgeo.2014.02.003.
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Basic information
Original name Mineral-forming and diagenetic processes related to Tertiary hydrocarbon seepage at the Bohemian Massif/Outer Western Carpathians interface: Evidence from the Hrabůvka quarry, Moravia, Czech Republic
Authors DOLNÍČEK, Zdeněk (203 Czech Republic), Tomáš LEHOTSKÝ (203 Czech Republic), Marek SLOBODNÍK (203 Czech Republic, guarantor, belonging to the institution), Eva HEJTMÁNKOVÁ (203 Czech Republic), Andrea GRÍGELOVÁ (203 Czech Republic) and Jan ZAPLETAL (203 Czech Republic).
Edition Marine and Petroleum Geology, Butterworth Scientific, 2014, 0264-8172.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher United Kingdom of Great Britain and Northern Ireland
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 2.639
RIV identification code RIV/00216224:14310/14:00073560
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.marpetgeo.2014.02.003
UT WoS 000334089300006
Keywords in English Moravo-Silesian Culm; Carpathian Foredeep; Hydrocarbons; Methane seep; Methane oxidation; Authigenic mineralization; REE
Tags AKR, rivok
Tags International impact, Reviewed
Changed by Changed by: Ing. Andrea Mikešková, učo 137293. Changed: 9/4/2015 21:29.
Abstract
Ancient hydrocarbon seepage occurred in the Hrabůvka quarry at the boundary between the basement of the Bohemian Massif (represented by folded Lower Carboniferous siliciclastics of the Culm facies) and Tertiary sedimentary cover of the Carpathian Foredeep (formed by Lower Badenian siliciclastics and calcareous clays). Mineralogical, stable isotope, elemental geochemical, and fluid inclusion data are presented in order to asses the origin of rocks, veins, and their fluids.
Abstract (in Czech)
V lomu Hrabůvka situovaném při hranici Českého masivu (reprezentovaným zvrásněnými spodnokarbonskými siliciklastiky kulmské facie) a terciérním sedimentárním pokryvem Západních Karpat (tvořeném spodnobadenskými siliciklastiky a vápnitými jíly) byl v geologickém záznamu zjištěn fosilní vývěr uhlovodíků. V článku jsou prezentovány mineralogické, izotopové a geochemické údaje a také data ze studia fluidních inkluzí, které umožnily vyhodnotit genezi daných hornin, žil a jejich fluid.
Links
GA205/00/0356, research and development projectName: Geochemický a tektonický model migrace fluid v paleozoiku moravskoslezské oblasti
Investor: Czech Science Foundation, Geochemical and tectonic model of fluid migration in the paleozoic of Moravo-Silesian region
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