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Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria)

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MILENKOV Georgi VASSILEVA Rossitsa D GEORGIEVA Sylvina KOUZMANOV Kalin CEMPÍREK Jan GEORGIEVA Yana

Rok publikování 2023
Druh Článek ve sborníku
Konference 17th Biennial SGA Meeting - Proceedings Volume 1
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www https://www.e-sga.org/fileadmin/PDF/Conference_proceedings/Zuerich/SGA_2023_Zurich_Volume_1.pdf
Klíčová slova Pegmatites; Central Rhodopes; Bulgaria; Critical elements
Popis Pegmatites are one of the main sources of some critical elements required for the 'green transition'. This specific lithology is commonly observed as a host rock for polymetallic mineralization in Pb-Zn deposits from the Central Rhodopes in Bulgaria. The main pegmatite-forming minerals are feldspar, quartz and mica. Allanite, titanite, zircon, monazite and apatite are commonly observed as accessory minerals. Despite no genetic relation between the Pb-Zn mineralization and the pegmatites, the latter are altered by the ore-forming fluids in these deposits. The hydrothermal alteration resulted in redistribution of various components to new minerals phases such as thorite, bastnasite, parisite, xenotime, REE-bearing clinozoisite and others.

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