Number of the records: 1  

Talc metasomatism of a magnesite body in response to a granite intrusion: Application of Sm–Nd dating of metasomatic dolomite

  1. 1.
    0582405 - GLÚ 2025 RIV NL eng J - Journal Article
    Majzlan, J. - Dianiška, I. - Kiefer, S. - Ackerman, Lukáš - Renčiuková, Veronika
    Talc metasomatism of a magnesite body in response to a granite intrusion: Application of Sm–Nd dating of metasomatic dolomite.
    Lithos. 470-471, April (2024), č. článku 107521. ISSN 0024-4937. E-ISSN 1872-6143
    Institutional support: RVO:67985831
    Keywords : Talc * Metasomatism * Magnesite * Permian granites * Western Carpathians
    OECD category: Geology
    Impact factor: 3.5, year: 2022
    Method of publishing: Limited access
    https://www.sciencedirect.com/science/article/pii/S0024493724000331?via%3Dihub

    The deposit Gemerská Poloma is located in the Gemeric Superunit of the Western Carpathians and it is currently mined for talc. Talc formed by metasomatic replacement of magnesite, together with dolomite, quartz, pyrite, and accessory minerals. Leachates of dolomite samples in 2.5 M acetic acid yield a Smsingle bondNd isochron age of 271 ± 7 Ma. This age coincides with the previously published ages of the underlying, evolved granitic rocks (from 265 ± 17 to 257 ± 5 Ma, U–Th–Pb on monazite) and the Usingle bondPb age of uraninite (264 ± 1 Ma) interpreted to form from fluids expelled during granite crystallization. The relationship of metasomatism and the granites is further supported by: (i) increased Li and F concentrations in the leachates from dolomite (when compared to the primary magnesite), (ii) increased total REE concentrations in dolomite (compared to magnesite) and even presence of individual REE minerals (bastnäsite) in the ore body, (iii) chondritic Y/Ho ratios, compatible with a magmatic source, (iv) the presence of skarn bodies directly above the magnesite-talc ore deposit, and (v) previously inferred low pressure of talc metasomatism, typical for contact metamorphism in shallow crustal levels. The positive europium anomalies argue for the metasomatism by the action of high-temperature (> 250 °C) hydrothermal fluids that progressively cooled below 250 °C. Thus, the observed talc metasomatism was triggered by the intrusion of the Permian granitic rocks. The Alpine processes tectonically modified the ore body, caused recrystallization and folding of the pre-existing talc and formation of new talc, and obliterated much of the evidence of the earlier processes.
    Permanent Link: https://hdl.handle.net/11104/0353085

     
     
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.