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

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F23%3A00142079" target="_blank" >RIV/00216224:14310/23:00142079 - isvavai.cz</a>
Result on the web
<a href="https://www.e-sga.org/fileadmin/PDF/Conference_proceedings/Zuerich/SGA_2023_Zurich_Volume_1.pdf" target="_blank" >https://www.e-sga.org/fileadmin/PDF/Conference_proceedings/Zuerich/SGA_2023_Zurich_Volume_1.pdf</a>
DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria)
Original language description
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.
Czech name
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Czech description
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Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2023
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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