J 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

Štítky

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.