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

0582405 - GLÚ 2025 RIV NL eng J - Článek v odborném periodiku
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
Institucionální podpora: RVO:67985831
Klíčová slova: Talc * Metasomatism * Magnesite * Permian granites * Western Carpathians
Obor OECD: Geology
Impakt faktor: 3.5, rok: 2022
Způsob publikování: Omezený přístup
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.
Trvalý link: https://hdl.handle.net/11104/0353085