Skarn association from pegmatite/marble contact in NW Rila:
occurrence and composition of F-enriched vesuvianite

J 2024

Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite

VASSILEVA, Rossitsa D; Svetoslav PETRUSSENKO; Sylvina GEORGIEVA; Jan CEMPÍREK; Radek ŠKODA et. al.

Základní údaje

Originální název

Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite

Autoři

VASSILEVA, Rossitsa D; Svetoslav PETRUSSENKO; Sylvina GEORGIEVA; Jan CEMPÍREK (203 Česká republika, domácí) a Radek ŠKODA (203 Česká republika, domácí)

Vydání

Review of the Bulgarian geological society, Bulgarian Academy of Sciences, 2024, 0007-3938

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Bulharsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 0.300

Kód RIV

RIV/00216224:14310/24:00138649

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.52215/rev.bgs.2024.85.2.128

UT WoS

001379096800027

Klíčová slova anglicky

Ca-skarn mineralization; fluorvesuvianite; trace elements; calc-silicate rocks; NW Rila

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 27. 1. 2025 11:15, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Calcic skarns are formed on the pegmatite/marble contact in the region of Dzhendemski Ezera, NW Rila, Bulgaria. The garnet/vesuvianite-dominated association is formed in the marbles of the Malyovitsa Lithotectonic Unit as a result of emplacement of crosscutting pegmatite injections. Large (up to 3 cm) prismatic vesuvianite crystals and their radiating aggregates are associated with garnet masses, diopside, scapolite, and zoisite. Representative samples were selected for mineralogical and geochemical study, focused on the vesuvianite composition and its associated minerals. Significant incorporation of fluorine is an important compositional characteristic in vesuvianite and garnet evidencing for the fluid/rock interaction and diffusion-involved bimetasomatic processes due to pegmatite intrusion. Trace-element signatures of the skarn minerals reveal constant isomorphic incorporation of large set of elements including V, Zn, Ga, Ge, Sn, Ni, Bi, REE, HFSE, U.

Citovat

VASSILEVA, Rossitsa D; Svetoslav PETRUSSENKO; Sylvina GEORGIEVA; Jan CEMPÍREK a Radek ŠKODA. Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite. Review of the Bulgarian geological society. Bulgarian Academy of Sciences, 2024, roč. 85, č. 2, s. 128-131. ISSN 0007-3938. Dostupné z: https://doi.org/10.52215/rev.bgs.2024.85.2.128.

@article{2471526,
   author = {Vassileva, Rossitsa D and Petrussenko, Svetoslav and Georgieva, Sylvina and Cempírek, Jan and Škoda, Radek},
   article_number = {2},
   doi = {https://doi.org/10.52215/rev.bgs.2024.85.2.128},
   keywords = {Ca-skarn mineralization; fluorvesuvianite; trace elements; calc-silicate rocks; NW Rila},
   language = {eng},
   issn = {0007-3938},
   journal = {Review of the Bulgarian geological society},
   title = {Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite},
   url = {https://bgd.bg/REVIEW_BGS/REVIEW_BGD_2024_2/PDF/17_Vassileva-2_REV-BGS_2024-2.pdf},
   volume = {85},
   year = {2024}
}

TY  - JOUR
ID  - 2471526
AU  - Vassileva, Rossitsa D - Petrussenko, Svetoslav - Georgieva, Sylvina - Cempírek, Jan - Škoda, Radek
PY  - 2024
TI  - Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite
JF  - Review of the Bulgarian geological society
VL  - 85
IS  - 2
SP  - 128-131
EP  - 128-131
PB  - Bulgarian Academy of Sciences
SN  - 00073938
KW  - Ca-skarn mineralization
KW  - fluorvesuvianite
KW  - trace elements
KW  - calc-silicate rocks
KW  - NW Rila
UR  - https://bgd.bg/REVIEW_BGS/REVIEW_BGD_2024_2/PDF/17_Vassileva-2_REV-BGS_2024-2.pdf
N2  - Calcic skarns are formed on the pegmatite/marble contact in the region of Dzhendemski Ezera, NW Rila, Bulgaria. The garnet/vesuvianite-dominated association is formed in the marbles of the Malyovitsa Lithotectonic Unit as a result of emplacement of crosscutting pegmatite injections. Large (up to 3 cm) prismatic vesuvianite crystals and their radiating aggregates are associated with garnet masses, diopside, scapolite, and zoisite. Representative samples were selected for mineralogical and geochemical study, focused on the vesuvianite composition and its associated minerals. Significant incorporation of fluorine is an important compositional characteristic in vesuvianite and garnet evidencing for the fluid/rock interaction and diffusion-involved bimetasomatic processes due to pegmatite intrusion. Trace-element signatures of the skarn minerals reveal constant isomorphic incorporation of large set of elements including V, Zn, Ga, Ge, Sn, Ni, Bi, REE, HFSE, U.
ER  -

VASSILEVA, Rossitsa D; Svetoslav PETRUSSENKO; Sylvina GEORGIEVA; Jan CEMPÍREK a Radek ŠKODA. Skarn association from pegmatite/marble contact in NW Rila: occurrence and composition of F-enriched vesuvianite. \textit{Review of the Bulgarian geological society}. Bulgarian Academy of Sciences, 2024, roč.~85, č.~2, s.~128-131. ISSN~0007-3938. Dostupné z: https://doi.org/10.52215/rev.bgs.2024.85.2.128.

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