Podrobnosti záznamu

Název
    Argillization of topaz-bearing granites in the Hub stock, Horní Slavkov-Krásno SN-W ore district (Bohemian Massif, Czech Republic)
Autor
    René, Miloš
    Šťastný, Martin
Jazyk
    anglicky
Typ dokumentu
    článek v odborném periodiku
Zdrojový dokument - seriál
    Acta geodynamica et geomaterialia
Svazek/č.
    Roč. 11, č. 3
Strany
    s. 255-267
Rok
    2014
Poznámky
    Projekt: GA205/09/0540, GA ČR3cav_un_auth*0253156
    Rozsah: 13 s. : P
Předmětová kategorie
    argillization
    Bohemian Massif
    clay minerals
    dickite
    Saxothuringian Zone
    topaz granite
    tosudite
Klíčové slovo
    Argillization
    Bohemian
    Czech
    District
    Granites
    Horní
    Hub
    Massif
    Ore
    Republic
    Slavkov-Krásno
    SN-W
    Stock
    Topaz-bearing
Abstrakt (anglicky)
   Argillized granites from the Hub stock contain a clay mineral assemblage formed by dickite, illite, tosudite and smectite. These granites occur in the upper part of the topaz granite stock, immediately beneath topaz-mica greisens consisting of quartz, clay minerals, lithium mica (protolithionite) and topaz. Argillized granites are enriched in Si (up to 78 wt.% SiO2), Fe (0.5-3 wt.% FeOtot.), F (up to 1.6 wt.%), Rb (830-1380 ppm), Li (515-2317 ppm), Nb (25-435 ppm) and Ta (21-64 ppm), but poor in Th (2-9 ppm), Zr (7-35 ppm) and bulk of REE (3-7 ppm). Newly recognized tosudite was identified on the basis of d (001) 29.4 Å XRD reflection on natural, oriented sample and 31.6 Å reflection after ethylene glycol treatment. The d (060) reflection appeared at 1.493 Å. The tosudite originated, according to fluid inclusion study of quartz from quartz veins at temperatures of 374-393 ºC.
   The hydrothermal activity of Li-enriched solutions, originated by muscovitization of Li-micas from greisenized topaz-albite granites and greisens was satisfactory for the formation of tosudite. The clay mineral assemblage (dickite, illite and smectite) originated, according to fluid inclusion study of fluorite, at temperatures ranging between 90 ºC and 185 ºC.
Přispěvatel
    AV ČR Brno, Ústav struktury minerálů a hornin
Kód přispěvatele
    AV ČR, ÚSMH
Zdrojový formát
    U
Datum importu
    24. 10. 2014