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Chemical and Textural Peculiarities of Zircon from Peralkaline Granites and Quartz-Bearing Syenites

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F41601670%3A_____%2F24%3AN0000006" target="_blank" >RIV/41601670:_____/24:N0000006 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/24:00582818

  • Result on the web

    <a href="https://www.mdpi.com/2075-163X/14/2/187" target="_blank" >https://www.mdpi.com/2075-163X/14/2/187</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3390/min14020187" target="_blank" >10.3390/min14020187</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Chemical and Textural Peculiarities of Zircon from Peralkaline Granites and Quartz-Bearing Syenites

  • Original language description

    Zircon from four plutons of peralkaline granites and quartz-bearing syenites, differing in geotectonic positions, petrological and mineralogical compositions, and contents of volatile and trace elements, was studied using SEM, CL, and EPMA with the intention to define typical textural and chemical features of zircon from peralkaline rocks. In strongly peralkaline Na-pyroxene-bearing rocks represented by the Khan Bogd and Khalzan Buregte plutons (Mongolia), the primary zircon is scarce or missing. Most zircon grains are secondary, originating in hydrothermal stage from primary Zr silicates. They often form globular or radial aggregates. Chemical compositions of zircon in these rocks typically show high contents of Y, moderate contents of REE (thus high Y/Yb values) together with low contents of U and Th and low analytical totals. In mildly peralkaline mica-bearing rocks represented by Ivigtut stock (Groenland) and Madeira pluton (Brazil), the exclusive primary Zr mineral is zircon, mostly of orthomagmatic origin. Its analytical totals approach 100 wt%, enrichment in HREE, resulting in low Y/Yb values, is typical. Zircon populations from two types of peralkaline granitoids can be distinguished from each other and from zircon from S-type granites based on combination of the Zr/Hf, Y/Yb, and U/Th values, or on the Y-Hf-P ternary diagram.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GX19-29124X" target="_blank" >GX19-29124X: EVOLUTION AND POST-EMPLACEMENT HISTORY OF CARBONATITES: IMPLICATIONS FOR THE MOBILITY AND CONCENTRATION OF CRITICAL METALS</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

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

    Minerals

  • ISSN

    2075-163X

  • e-ISSN

  • Volume of the periodical

    14/2

  • Issue of the periodical within the volume

    187

  • Country of publishing house

    CH - SWITZERLAND

  • Number of pages

    29

  • Pages from-to

  • UT code for WoS article

    001172207800001

  • EID of the result in the Scopus database