LOSOS, Zdeněk, Ondřej KOVÁŘ, Stanislav HOUZAR and Josef ZEMAN. Rare hydrated Mg-carbonates-hydroxides assemblage of serpentinite fissures in Hrubšice, western Moravia (Czech Republic): a genetic model of its formation. Neues Jahrbuch fur Mineralogie, Abhandlungen. Stuttgart, 2013, vol. 190, No 3, p. 253-263. ISSN 0077-7757. Available from: https://dx.doi.org/10.1127/0077-7757/2013/0242.
Other formats:   BibTeX LaTeX RIS
Basic information
Original name Rare hydrated Mg-carbonates-hydroxides assemblage of serpentinite fissures in Hrubšice, western Moravia (Czech Republic): a genetic model of its formation
Authors LOSOS, Zdeněk (203 Czech Republic, guarantor, belonging to the institution), Ondřej KOVÁŘ (203 Czech Republic, belonging to the institution), Stanislav HOUZAR (203 Czech Republic) and Josef ZEMAN (203 Czech Republic, belonging to the institution).
Edition Neues Jahrbuch fur Mineralogie, Abhandlungen, Stuttgart, 2013, 0077-7757.
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: 0.857
RIV identification code RIV/00216224:14310/13:00072036
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1127/0077-7757/2013/0242
UT WoS 000322766800002
Keywords in English artinite;hydromagnesite;brugnatellite;coalingite;fissure minerals;Raman spectrum;serpentinite;Moldanubicum;Bohemian Massif
Tags AKR, rivok
Tags International impact, Reviewed
Changed by Changed by: doc. RNDr. Zdeněk Losos, CSc., učo 2470. Changed: 12/2/2014 14:24.
Abstract
Low-temperature fissure Mg- (Fe-) hydrocarbonate mineralization was found in the Hrubšiceserpentinite body, Moravian Moldanubicum. It is formed by rare minerals (hydromagnesite, artinite, brugnatellite, coalingite), followed by aragonite, brucite, dolomite and calcite. Two main stages of crystallization have been recognised. The old stage of mineralization was relatively Fe-rich, with brugnatellite, coalingite and Fe-bearing brucite. The younger, more extensive Mg-rich stage, produced artinite and various morphological types of hydromagnesite. The youngest minerals of fissures are calcite, dolomite and aragonite. Mineral assemblages have formed from low-temperature solutions, which were enriched in Mg2+, at pH ~ 9, with relatively low Al activity, low fugacity of CO2 and temperature lower than 44 oC.
PrintDisplayed: 1/10/2024 10:23