Počet záznamů: 1  

The involvement of F CO.sub.2./sub., and As in the alteration of Zr-Th-REE-bearing accessory minerals in a the Hora Svaté Kateřiny A-type granite, Czech Republic

  1. 1.
    SYSNO ASEP0338926
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevThe involvement of F CO2, and As in the alteration of Zr-Th-REE-bearing accessory minerals in a the Hora Svaté Kateřiny A-type granite, Czech Republic
    Tvůrce(i) Breiter, Karel (GLU-S) RID, SAI, ORCID
    Čopkajová, R. (CZ)
    Škoda, R. (CZ)
    Zdroj.dok.Canadian Mineralogist. - : Mineralogical Association of Canada - ISSN 0008-4476
    Roč. 47, č. 6 (2009), s. 1375-1398
    Poč.str.24 s.
    Forma vydáníWWW - WWW
    Jazyk dok.eng - angličtina
    Země vyd.CA - Kanada
    Klíč. slovazircon ; thorite ; monazite ; xenotime ; håleniusite ; granite ; solid solution ; Erzgebirge ( Czech Republic)
    Vědní obor RIVDB - Geologie a mineralogie
    CEPIAA300130801 GA AV ČR - Akademie věd
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000274017700005
    EID SCOPUS77249098367
    DOI10.3749/canmin.47.6.1375
    AnotaceThe assemblage of Zr(Hf)-Th(U)-REE minerals from an A-type granite from Hora Svaté Kateřiny were studied to distinguish magmatic and hydrothermal processes affected the rock. The primary accessory phases included fluorite, magnetite, zircon, xenotime, monazite, and thorite. Solid solutions of (Th+U)-, (Zr+Hf)- and REE-components formed domains within zircon and thorite crystals and are supposed to by primary. Pyrite and arsenopyrite crystallised from the first portion of hydrothermal fluid with low oxygen fugacity. Later, fluid with higher oxygen fugacity altered magnetite, sulphides, and dissolved xenotime. During this time, Th and U-bearing zircon and thorite were partially metamictised. Arsenic was oxidised to As5+ and intensively metasomatised xenotime, Y-rich zircon and thorite forming chernovite. Even later, fluid rich in CO2 dissolved metamictised thorite and partially dissolved monazite after only short transport at the contact with fluorite crystallised Th-rich bastnäsite.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2010
Počet záznamů: 1  

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