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Preliminary study of scandium enrichment in Çaldağ-Manisa lateritic Ni-Co deposit, Western Anatolia

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F24%3A00601230" target="_blank" >RIV/67985891:_____/24:00601230 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.17824/yerbilimleri.1491285" target="_blank" >https://doi.org/10.17824/yerbilimleri.1491285</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.17824/yerbilimleri.1491285" target="_blank" >10.17824/yerbilimleri.1491285</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Preliminary study of scandium enrichment in Çaldağ-Manisa lateritic Ni-Co deposit, Western Anatolia

  • Original language description

    Scandium is one of the most valuable critical metals, with high demand in applications ranging from biomedical research to electronics. Lateritic Ni-Co deposits are considered prime targets for scandium (Sc) exploration because Sc can be concentrated during weathering through residual and secondary enrichment, reaching up to 100 ppm and making it a potential by-product.nThis study investigates the distribution of Sc in the unweathered parent rocks and various laterite zones within two distinct pits of the Çaldağ lateritic Ni-Co deposit in Western Anatolia. In the Hematite pit, the serpentinite protolith shows an average Sc content of 10.3 ppm, with significant enrichment in the middle-upper limonite zone, reaching up to ~66 ppm. Although this represents a sixfold increase compared to the serpentinite protolith, the maximum Sc concentrations (53.6–65.7 ppm) are relatively low compared to other nickel laterites with by-product Sc potential (~100 ppm). This lower concentration is attributed to the initial low Sc content of the serpentinized peridotite protolith and post-lateritization tectonic activity. Conversely, the South pit exhibits higher initial Sc content in the protolith (~13 ppm) but lower average Sc content (~6.4 ppm) in the limonite zone, likely due to post-lateritization dissolution of Sc-hosting minerals by alteration and secondary weathering processes within the highly deformed pit.nThe findings suggest that while the Çaldağ deposit exhibits Sc concentrations up to ~66 ppm in the limonite zones, the potential for Sc as a by-product alongside Ni production is limited. Further detailed mineralogical and geochemical investigations are recommended to gain a deeper understanding of the mechanisms of Sc distribution in the Çaldağ deposit and other lateritic deposits in Türkiye.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>SC</sub> - Article in a specialist periodical, which is included in the SCOPUS database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    YERBİLİMLERİ/Bulletin for Earth Sciences

  • ISSN

    1301-2894

  • e-ISSN

    2687-2978

  • Volume of the periodical

    45

  • Issue of the periodical within the volume

    3

  • Country of publishing house

    TR - TURKEY

  • Number of pages

    22

  • Pages from-to

    1491285

  • UT code for WoS article

  • EID of the result in the Scopus database

    2-s2.0-85214931122