Počet záznamů: 1  

Laser ablation ICPMS study of trace element chemistry in molybdenite coupled with scanning electron microscopy (SEM) - An important tool for identification of different types of mineralization

  1. 1.
    SYSNO ASEP0460127
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevLaser ablation ICPMS study of trace element chemistry in molybdenite coupled with scanning electron microscopy (SEM) - An important tool for identification of different types of mineralization
    Tvůrce(i) Pašava, J. (CZ)
    Svojtka, Martin (GLU-S) SAI, RID, ORCID
    Veselovský, F. (CZ)
    Ďurišová, Jana (GLU-S) RID, SAI
    Ackerman, Lukáš (GLU-S) RID, SAI, ORCID
    Pour, O. (CZ)
    Drábek, M. (CZ)
    Halodová, P. (CZ)
    Haluzová, Eva (GLU-S) RID, SAI
    Zdroj.dok.Ore Geology Reviews. - : Elsevier - ISSN 0169-1368
    Roč. 72, č. 1 (2016), s. 874-895
    Poč.str.22 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.NL - Nizozemsko
    Klíč. slovamolybdenite ; trace-element geochemistry ; Laser Ablation Inductively Coupled Mass ; spectrometry ; scanning electron microscopy ; nano- to micro-inclusions ; Bohemian Massif ; Uzbekistan
    Vědní obor RIVDB - Geologie a mineralogie
    CEPGA13-15390S GA ČR - Grantová agentura ČR
    Institucionální podporaGLU-S - RVO:67985831
    UT WOS000366345100050
    EID SCOPUS84942749627
    DOI10.1016/j.oregeorev.2015.09.007
    AnotaceUsing the example of four different types of associations from the Bohemian Massif (greisen-, gold-, base metal-, and "barren granite"-related) and of one porphyry-Cu-Mo(Au) deposit from Uzbekistan, it is shown that molybdenite from a specific type of mineralization possesses a distinct trace-element geochemical composition, which is locally influenced by the presence of relevant mineral phases occurring in the form of sub-nano-, nano-to micron-scale impurities/inclusions. It is documented that, besides typically lattice-bound elements (Re, and W) and isostructural concentrations of Se and Te (substituting for S), molybdenite can concentrate other metals (e.g., Ag, As, Au, Bi, Cu, Nb, Pb, Zn, Zr) which mostly form inclusions or impurities. The distribution of Re in molybdenite indicates crustal sources for the group of greisen-, base-metal-, and a few of the granite-related deposits, compared to a mixed mantle/crustal source for the Au-related and majority of granite-related deposits. Molybdenite from the Kalmakyr porphyry-Cu-Mo (Au) deposit in Uzbekistan is characterized by the highest mean Re value (236 ppm). Rhenium, Se and W have a homogeneous distribution in molybdenite from this deposit. Only galena and anglesite inclusions were identified visually in molybdenite from this type of deposit, while the presence of most likely sub-nano impurities of Cu, Zn and Ag is indicated by LA-ICPMS time-resolved depth profiles.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2017
Počet záznamů: 1  

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