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Evolution of rare-metal granitic magmas documented by quartz chemistry

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    SYSNO ASEP0323734
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleEvolution of rare-metal granitic magmas documented by quartz chemistry
    TitleVývoj rudonosných granitových magmat dokumentovaný chemickým složením křemene
    Author(s) Breiter, Karel (GLU-S) RID, SAI, ORCID
    Müller, A. (NO)
    Source TitleEuropean Journal of Mineralogy. - : Copernicus - ISSN 0935-1221
    Roč. 21, č. 2 (2009), s. 335-346
    Number of pages12 s.
    Publication formWWW - WWW
    Languageeng - English
    CountryDE - Germany
    Keywordsquartz ; LA-ICP-MS ; trace element analysis ; rare metal granite ; Erzgebirge/ Krušné Hory
    Subject RIVDB - Geology ; Mineralogy
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000265595000006
    EID SCOPUS67649497717
    DOI10.1127/0935-1221/2009/0021-1907
    AnnotationThe study documents changes in the chemical composition of igneous quartz during evolution of two contrasting late-Variscan granite suites in the Erzgebirge/Krušné Hory Mts., Czech Republic. Contents of Li, Be, B, Al, Ge, P, K, Na, Ca, Ti, Mn, and Fe were determined in situ using LA-ICP-MS. Al reached the highest contents in all samples (100-1200 ppm), followed by Ti, Li, and K (in the range of 10-100 ppm). The contents of B, Be, Ge, Fe, Mn, and P in quartz are usually lower than 10 ppm. The Ti versus Al diagram is the most fitting indicator of the evolution of the melt from which the quartz crystallised.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2009
Number of the records: 1  

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