Podrobnosti záznamu

Název
    Extreme variation and apparent reversal of Nb-Ta fractionation in columbite-group minerals from the Scheibengraben beryl-columbite granitic pegmatite, Maršíkov, Czech Republic
Údaj o odpovědnosti
    Milan Novák, Petr Černý
Autor
    Černý, Petr
    Novák, Milan, 1952-
    Uher, Pavel
Jazyk
    anglicky
Zdrojový dokument - seriál
    European journal of mineralogy
Svazek/č.
    Vol. 15, no. 3
Strany
    p. 565-574
Rok
    2003
Poznámky
    5 obr., 2 tab.
    il.
    Obsahuje bibliografické odkazy
    Zkr. název ser.: Eur. J. Mineral.
Předmětová skupina
    chemismus minerálů
    fluor
    frakcionace chemická
    mangan
    niob
    pegmatit
    silesikum
    skupina columbitu
    tantal
    železo
Geografické jméno
    ČR-Morava
    Maršíkov (Šumperk)
Klíčové slovo
    Apparent
    Beryl-columbite
    Columbite-group
    Czech
    Extreme
    Fractionation
    Granitic
    Maršíkov
    Minerals
    Nb-Ta
    Pegmatite
    Republic
    Reversal
    Scheibengraben
    Variation
Abstrakt (anglicky)
   Compositional variation was studied in columbite-group minerals from the beryl-columbite pegmatite at Scheibengraben, Maršíkov, Northern Moravia, Czech Republic. The pegmatite consists of five textural-paragenetic units, from the least to the most evolved: volumetrically dominant coarse-grained unit, subordinate graphic and blocky units and a minor cleave-landite unit; a saccharoidal albite unit is rather randomly distributed within the dike. It replaces and/or crosscuts all other units except the cleavelandite unit. Columbite-group minerals are the dominant Nb,Ta-oxide phases in all units. They are associated with other Nb,Ta-oxide minerals: minerals of the pyrochlore subgroup and fersmite in the coarse-grained unit, and minerals of the microlite subgroup, ferrotapiolite and rynersonite in the cleavelandite unit.
   The extreme Nb-Ta [Ta/(Ta+Nb) = 0.06 to 0.97 (microlite 0.99)] and appreciable Fe-Mn [Mn/(Mn+Fe) = (ferrotapiolite 0.22) 0.35 to 0.90] fractionations in columbite-group minerals differ from those observed in beryl pegmatites examined to date, but they are comparable with those in some highly fractionated, complex, Li-rich pegmatites. High activity of F (facilitated by low contents of B, P and Li in the pegmatite melt) very likely maximized such an extensive Nb-Ta fractionation, over and above differential solubilities of columbite and tantalite in pegmatite melt. The apparent reversal of Nb-Ta and Fe-Mn fractionations found in columbite from the saccharoidal albite unit seems to be an artefact from early units (particularly the coarse-grained one), which were extensively replaced by saccharoidal albite
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    15. 8. 2007
Datum importu
    8. 8. 2012