Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral
Composition and Retrograde Alteration

J 2025

Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration

VASSILEVA, Rossitsa D.; Sylvina GEORGIEVA; Georgi MILENKOV; Yana GEORGIEVA; Radek ŠKODA et al.

Základní údaje

Originální název

Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration

Autoři

VASSILEVA, Rossitsa D.; Sylvina GEORGIEVA; Georgi MILENKOV; Yana GEORGIEVA; Radek ŠKODA; Jan CEMPÍREK a Danail YOVCHEV

Vydání

COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES, SOFIA, PUBL HOUSE BULGARIAN ACAD SCI, 2025, 1310-1331

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10504 Mineralogy

Stát vydavatele

Bulharsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 0.300 v roce 2024

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/25:00143361

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

diopside; olivine; base metal deposits; Central Rhodopes; Laki ore district

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 2. 4. 2026 13:17, Mgr. Petra Trembecká, Ph.D.

Anotace

V originále

The studied diopside-forsterite skarn from the Djurkovo base metal deposit formed through high-temperature metasomatic processes between dolomitic marble and fluids associated with a thin pegmatite dyke. Early prograde stages involved decarbonation reactions and SiO2 addition, resulting in diopside and forsterite deposition, followed by phlogopite crystallization. Subsequent retrograde alteration replaced primary minerals with tremolite, serpentine, talc, and chlorite, the latter indicating precipitation temperatures at ti 260 degrees C. Mineral assemblages and textures reflect a multistage evolution involving progressive hydration and oxidation (evidenced by troilite/magnetite transformation). Trace element geochemistry reveals incorporation of Li, B, Zn, Ga, V, Cr, Cs, Y, and Nb, generally concentrated in retrograde phases. Despite the lack of economic mineralization, the geochemical signatures of the studied skarn provide insights into fluid evolution and mineral-forming processes and may assist in broader exploration within the Central Rhodopean metallogenic province.

Citovat

VASSILEVA, Rossitsa D.; Sylvina GEORGIEVA; Georgi MILENKOV; Yana GEORGIEVA; Radek ŠKODA; Jan CEMPÍREK a Danail YOVCHEV. Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration. COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES. SOFIA: PUBL HOUSE BULGARIAN ACAD SCI, 2025, roč. 78, č. 11, s. 1655-1668. ISSN 1310-1331. Dostupné z: https://doi.org/10.7546/CRABS.2025.11.09.

@article{2547549,
   author = {Vassileva, Rossitsa D. and Georgieva, Sylvina and Milenkov, Georgi and Georgieva, Yana and Škoda, Radek and Cempírek, Jan and Yovchev, Danail},
   article_location = {SOFIA},
   article_number = {11},
   doi = {https://doi.org/10.7546/CRABS.2025.11.09},
   keywords = {diopside; olivine; base metal deposits; Central Rhodopes; Laki ore district},
   language = {eng},
   issn = {1310-1331},
   journal = {COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES},
   title = {Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration},
   url = {https://www.proceedings.bas.bg/index.php/cr/article/view/877},
   volume = {78},
   year = {2025}
}

TY  - JOUR
ID  - 2547549
AU  - Vassileva, Rossitsa D. - Georgieva, Sylvina - Milenkov, Georgi - Georgieva, Yana - Škoda, Radek - Cempírek, Jan - Yovchev, Danail
PY  - 2025
TI  - Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration
JF  - COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES
VL  - 78
IS  - 11
SP  - 1655-1668
EP  - 1655-1668
PB  - PUBL HOUSE BULGARIAN ACAD SCI
SN  - 13101331
KW  - diopside
KW  - olivine
KW  - base metal deposits
KW  - Central Rhodopes
KW  - Laki ore district
UR  - https://www.proceedings.bas.bg/index.php/cr/article/view/877
N2  - The studied diopside-forsterite skarn from the Djurkovo base metal deposit formed through high-temperature metasomatic processes between dolomitic marble and fluids associated with a thin pegmatite dyke. Early prograde stages involved decarbonation reactions and SiO2 addition, resulting in diopside and forsterite deposition, followed by phlogopite crystallization. Subsequent retrograde alteration replaced primary minerals with tremolite, serpentine, talc, and chlorite, the latter indicating precipitation temperatures at ti 260 degrees C. Mineral assemblages and textures reflect a multistage evolution involving progressive hydration and oxidation (evidenced by troilite/magnetite transformation). Trace element geochemistry reveals incorporation of Li, B, Zn, Ga, V, Cr, Cs, Y, and Nb, generally concentrated in retrograde phases. Despite the lack of economic mineralization, the geochemical signatures of the studied skarn provide insights into fluid evolution and mineral-forming processes and may assist in broader exploration within the Central Rhodopean metallogenic province.
ER  -

VASSILEVA, Rossitsa D.; Sylvina GEORGIEVA; Georgi MILENKOV; Yana GEORGIEVA; Radek ŠKODA; Jan CEMPÍREK a Danail YOVCHEV. Magnesian Skarns from the Djurkovo Pb-Zn Deposit: Mineral Composition and Retrograde Alteration. \textit{COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES}. SOFIA: PUBL HOUSE BULGARIAN ACAD SCI, 2025, roč.~78, č.~11, s.~1655-1668. ISSN~1310-1331. Dostupné z: https://doi.org/10.7546/CRABS.2025.11.09.

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