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

D 2023

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

MILENKOV, Georgi; Rossitsa D VASSILEVA; Sylvina GEORGIEVA; Kalin KOUZMANOV; Jan CEMPÍREK et. al.

Základní údaje

Originální název

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

Autoři

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

Vydání

Geneva, 17th Biennial SGA Meeting - Proceedings Volume 1, od s. 278-281, 4 s. 2023

Nakladatel

Society for Geology Applied to Mineral Deposits

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10505 Geology

Stát vydavatele

Švýcarsko

Utajení

není předmětem státního či obchodního tajemství

Forma vydání

tištěná verze "print"

Odkazy

URL

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-2-8399-4044-3

UT WoS

001238045900074

Klíčová slova anglicky

Pegmatites; Central Rhodopes; Bulgaria; Critical elements

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 22. 9. 2025 10:45, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

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.

Citovat

MILENKOV, Georgi; Rossitsa D VASSILEVA; Sylvina GEORGIEVA; Kalin KOUZMANOV; Jan CEMPÍREK a Yana GEORGIEVA. Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria). In Chelle-Michou Cyril, Saintilan Nicolas. 17th Biennial SGA Meeting - Proceedings Volume 1. Geneva: Society for Geology Applied to Mineral Deposits, 2023, s. 278-281. ISBN 978-2-8399-4044-3.

@inproceedings{2520457,
   author = {Milenkov, Georgi and Vassileva, Rossitsa D and Georgieva, Sylvina and Kouzmanov, Kalin and Cempírek, Jan and Georgieva, Yana},
   address = {Geneva},
   booktitle = {17th Biennial SGA Meeting - Proceedings Volume 1},
   editor = {Chelle-Michou Cyril, Saintilan Nicolas},
   keywords = {Pegmatites; Central Rhodopes; Bulgaria; Critical elements},
   howpublished = {tištěná verze "print"},
   language = {eng},
   location = {Geneva},
   isbn = {978-2-8399-4044-3},
   pages = {278-281},
   publisher = {Society for Geology Applied to Mineral Deposits},
   title = {Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria)},
   url = {https://www.e-sga.org/fileadmin/PDF/Conference_proceedings/Zuerich/SGA_2023_Zurich_Volume_1.pdf},
   year = {2023}
}

TY  - CONF
ID  - 2520457
AU  - Milenkov, Georgi - Vassileva, Rossitsa D - Georgieva, Sylvina - Kouzmanov, Kalin - Cempírek, Jan - Georgieva, Yana
PY  - 2023
TI  - Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria)
PB  - Society for Geology Applied to Mineral Deposits
CY  - Geneva
SN  - 9782839940443
KW  - Pegmatites
KW  - Central Rhodopes
KW  - Bulgaria
KW  - Critical elements
UR  - https://www.e-sga.org/fileadmin/PDF/Conference_proceedings/Zuerich/SGA_2023_Zurich_Volume_1.pdf
N2  - 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.
ER  -

MILENKOV, Georgi; Rossitsa D VASSILEVA; Sylvina GEORGIEVA; Kalin KOUZMANOV; Jan CEMPÍREK a Yana GEORGIEVA. Comparative study of pegmatites from the Central Rhodopean Pb-Zn deposits (Bulgaria). In Chelle-Michou Cyril, Saintilan Nicolas. \textit{17th Biennial SGA Meeting - Proceedings Volume 1}. Geneva: Society for Geology Applied to Mineral Deposits, 2023, s.~278-281. ISBN~978-2-8399-4044-3.

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