2024
Incompatible Elements (REE, Th, U, Nb, Ta, Ti) Mineral Association in Altered Pegmatite from the Djurkovo Pb-Zn Deposit, Central Rhodopes: Occurrence and Geochemical Properties
GEORGIEVA, Sylvina; Rossitsa D VASSILEVA; Valentin GROZDEV; Georgi MILENKOV; Jan CEMPÍREK et. al.Základní údaje
Originální název
Incompatible Elements (REE, Th, U, Nb, Ta, Ti) Mineral Association in Altered Pegmatite from the Djurkovo Pb-Zn Deposit, Central Rhodopes: Occurrence and Geochemical Properties
Autoři
GEORGIEVA, Sylvina; Rossitsa D VASSILEVA; Valentin GROZDEV; Georgi MILENKOV; Jan CEMPÍREK; Radek ŠKODA a Elitsa STEFANOVA
Vydání
Comptes Rendus de L'Academie Bulgare des Sciences, Sofia, Academic Publishing House, 2024, 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
Impakt faktor
Impact factor: 0.300
Kód RIV
RIV/00216224:14310/24:00138005
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001346321100007
EID Scopus
2-s2.0-85208731922
Klíčová slova anglicky
(REE; U; Th)-(Nb; Ta; Ti) oxide minerals; ishikawaite; fergu- sonite; fersmite; thortveitite
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 13. 12. 2024 09:57, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
The Djurkovo base-metal vein deposit in Laki ore field, is hosted by a heterogeneous gneiss/amphibolite/marble rock sequence of the high-grade metamorphic complex of the Central Rhodopes. Mineralogical and geochemical investigation was conducted on slightly deformed, and hydrothermally altered thin pegmatite dykes intruded in the marbles. The pegmatite bodies consist mostly of K-feldspar, albite and quartz, with minor garnet present. Clear textural zonation within the bodies is absent except for the preferential crystallization of garnet in the innermost parts. The main pegmatite accessories include ishikawaite, zircon, apatite, monazite-(Ce), allanite-(Ce), and titanite. The post-magmatic hydrothermal overprint on the pegmatites resulted in the formation of the assemblage including epidote, sericite, chlorite, carbonate, quartz, hematite, and leucoxene. The accessory oxide, silicate, and phosphate minerals bearing rare earth elements (REE), actinides (ACT), Nb, Ta, and Ti have undergone partial replacement by secondary mineral phases (thortveitite, fergusonite, fersmite, uraninite, thorianite, REE-epidote, xenotime) observed as irregular grains or veinlets along fractures and dissolved zones, either inside or near the primary minerals.