BREITER, Karel, Jana ĎURIŠOVÁ, Tomáš HRSTKA, Zuzana KORBELOVÁ, Michaela HLOŽKOVÁ, Michaela VAŠINOVÁ GALIOVÁ, Viktor KANICKÝ, Petr RAMBOUSEK, Ilja KNÉSL, Petr DOBEŠ and Marek DOSBABA. Assessment of magmatic vs. metasomatic processes in rare-metal granites: A case study of the Cínovec/Zinnwald Sn – W – Li deposit, Central Europe. Lithos. Elsevier, 2017, vol. 292, November, p. 198-217. ISSN 0024-4937. Available from: https://dx.doi.org/10.1016/j.lithos.2017.08.015.
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Basic information
Original name Assessment of magmatic vs. metasomatic processes in rare-metal granites: A case study of the Cínovec/Zinnwald Sn – W – Li deposit, Central Europe
Authors BREITER, Karel (203 Czech Republic, guarantor), Jana ĎURIŠOVÁ (703 Slovakia), Tomáš HRSTKA (203 Czech Republic), Zuzana KORBELOVÁ (203 Czech Republic), Michaela HLOŽKOVÁ (203 Czech Republic, belonging to the institution), Michaela VAŠINOVÁ GALIOVÁ (203 Czech Republic, belonging to the institution), Viktor KANICKÝ (203 Czech Republic, belonging to the institution), Petr RAMBOUSEK (203 Czech Republic), Ilja KNÉSL (203 Czech Republic), Petr DOBEŠ (203 Czech Republic) and Marek DOSBABA (203 Czech Republic).
Edition Lithos, Elsevier, 2017, 0024-4937.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10406 Analytical chemistry
Country of publisher Norway
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 3.857
RIV identification code RIV/00216224:14310/17:00095003
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.lithos.2017.08.015
UT WoS 000416185500013
Keywords in English Rare-metal granite; Cínovec/Zinnwald deposit; Rock textures; Metasomatic processes; Magmatic processes
Tags NZ, rivok
Changed by Changed by: Ing. Nicole Zrilić, učo 240776. Changed: 28/3/2018 16:37.
Abstract
The Cínovec rare-metal granite in the eastern segment of the Krušné Hory/Erzgebirge (Czech Republic/Germany)formed in the final stage of the magmatic evolution of the late Variscan volcano-plutonic system known as the Teplice caldera. The granite is slightly peraluminous; enriched in F, Li, Rb, Cs, Nb, Ta, Sn, W, Sc and U; and poor in P, Mg, Ti, Sr and B.
Links
GA14-13600S, research and development projectName: Otevřené procesy v granitoidech z pohledu zonality minerálů a horninových textur
Investor: Czech Science Foundation
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