DOLNÍČEK, Zdeněk, Bohuslav FOJT, Walter PROCHASKA, Jan KUČERA and Petr SULOVSKÝ. Origin of the Zálesí U-Ni-Co-As-Ag/Bi deposit, Bohemian Massif, Czech Republic: Fluid inclusion and stable isotope constraints. Mineralium Deposita. 2009, vol. 44, No 1, p. 81-97. ISSN 0026-4598. Available from: https://dx.doi.org/10.1007/s00126-008-0202-6.
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Basic information
Original name Origin of the Zálesí U-Ni-Co-As-Ag/Bi deposit, Bohemian Massif, Czech Republic: Fluid inclusion and stable isotope constraints
Authors DOLNÍČEK, Zdeněk (203 Czech Republic), Bohuslav FOJT (203 Czech Republic, guarantor, belonging to the institution), Walter PROCHASKA (642 Romania), Jan KUČERA (203 Czech Republic, belonging to the institution) and Petr SULOVSKÝ (203 Czech Republic).
Edition Mineralium Deposita, 2009, 0026-4598.
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 Germany
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.520
RIV identification code RIV/00216224:14310/09:00056630
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1007/s00126-008-0202-6
UT WoS 000261692000006
Keywords (in Czech) Český Masív; Zálesí; Česká republika; pěti prvková asiociace; urán, fluidní inkluze; stabilní izotopy
Keywords in English Bohemian Massif; Zálesí; Czech Republic; Five-element association; Uranium; Fluid inclusions; Stable isotopes
Tags IK, rivok
Changed by Changed by: Mgr. Tomáš Marhanský, učo 356572. Changed: 30/3/2012 12:09.
Abstract
Abstract The Zálesí vein-type deposit is hosted by Early Paleozoic high-grade metamorphic rocks on the northern margin of the Bohemian Massif. The mineralization is composed of three main stages: uraninite, arsenide, and sulfide. The mineral assemblages formed at low temperatures and low pressures.
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