Podrobnosti záznamu

Název
    The chemical composition of REE-Y-Th-U-rich accessory minerals in peraluminous granites of the Erzgebirge-Fichtelgebirge region, Germany. Part II: Xenotime
Údaj o odpovědnosti
    Hans-Jürgen Förster
Autor
    Förster, Hans-Jürgen, 1948-
Jazyk
    anglicky
Zdrojový dokument - seriál
    American mineralogist
Svazek/č.
    Vol. 83, no. 11-12
Rok
    1998
Poznámky
    1 obr., 6 diagr., 2 tab., 2 s.bibl.
    Zkr. název ser.: Amer. Mineralogist
Předmětová skupina
    granit
    krušnohorský pluton
    krystalizace
    minerály akcesorické
    vzácné zeminy
    xenotim
Geografické jméno
    Cínovec (Teplice)
    ČR-Čechy
    SRN-Sachsen
Klíčové slovo
    Accessory
    Chemical
    Composition
    Erzgebirge-Fichtelgebirge
    Germany
    Granites
    II
    Minerals
    Peraluminous
    REE-Y-Th-U-rich
    Region
    Xenotime
Abstrakt (anglicky)
   enotime, from a geochemically heterogenous series of mildly to strongly peraluminous granites of the Erzgebirge, Germany, displays extended compositional variability with respect to abundances of HREE, Y, U, and Th. With few exceptions, the maximum and minimum concentrations for the lanthanides and actinides exceed those noted for this mineral from other geologic environments. Xenotime chemistry is dominated by the theoretical end-members HREE-PO4 and YPO4 (90 mol% in total). Typical xenotime grains from the Erzgebirge granites and from other granites worldwide contain 70-80 mol% YPO4, and 16-25 mol% HREE-PO4. This study documents the occurrence of xenotime, abnormally rich in HREE in place of Y, with up to 45 mol% HREE-PO4. Substitutions of thorite-coffinite, (Th, U, Pb) SiO4, brabantite, (Ca, Th, U) (PO4)2, and monazite, (La-Sm) PO4, are of minor importance, reaching maximum levels of 5-6 mol% each with a total contribution typically <10 mol%.
   Typically, the incorporation of actinides in xenotime from these and other granites, as well as from other rocks, is dominated by thorite-coffinite substitutions. However, in some xenotime grains, the U and Th concentrations are largely accounted for by the substitution mechanism 2 (REE, Y)3+ - (Th, U)4+ + Ca2+. The total lanthanide and actinide contents in xenotime and host granite are not strongly correlated. However, formation of xenotime unusually rich in HREE occurs only in the A-type Limica granites that are strongly enriched in these elements. The shapes of HREE patterns of xenotime and host are similar which, combined with mass-balance calculations, indicate the importance of this mineral in affecting the HREE as well as Y evolution of late-stage granitic melts.
   Late xenotime may show strong Y/Ho fractionation, thus recording the decoupling of Y and the HREE, which can occur in the latest stages of crystallization of evolved granites and which may be associated with deuteric alteration
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    18. 2. 2008
Datum importu
    8. 8. 2012