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REY plus ACT redistribution in polymineral aggregates: a case study on monazite decomposition in pegmatite

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VASSILEVA Rossitsa D GEORGIEVA Sylvina CEMPÍREK Jan MILENKOV Georgi ŠKODA Radek

Rok publikování 2024
Druh Článek v odborném periodiku
Časopis / Zdroj Review of the Bulgarian Geological Society
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace VASSILEVA, Rossitsa D, Sylvina GEORGIEVA, Jan CEMPÍREK, Georgi MILENKOV a Radek ŠKODA. REY plus ACT redistribution in polymineral aggregates: a case study on monazite decomposition in pegmatite. Review of the Bulgarian Geological Society. Bulgarian Academy of Sciences, 2024, roč. 85, č. 3, s. 124-127. ISSN 0007-3938. Dostupné z: https://dx.doi.org/10.52215/rev.bgs.2024.85.2.124.
www https://bgd.bg/REVIEW_BGS/REVIEW_BGD_2024_2/PDF/16_Vassileva-1_REV-BGS_2024-2.pdf
Doi http://dx.doi.org/10.52215/rev.bgs.2024.85.2.124
Klíčová slova pegmatite; monazite-(Ce); allanite-(Ce); complex multimineral aggregates
Popis Selected pegmatite dyke intruded within the gneiss-marble-amphibolite sequence of the Rhodope Metamorphic Complex was studied for its REY+ACT mineralization in attempt to assess the potential of these pegmatites for critical and strategic raw materials. Mineral composition of K-feldspar and albite is complemented by abundant common accessories of zircon, apatite, monazite, allanite, and titanite. The REY+ACT mineralization is presented as single euhedral crystals (zircon, thorianite, Y-Nb oxide, titanite and fluorapatite) or as complex multimineral nodule-like aggregates. The nodule core typically consists of decomposed Th-bearing monazite-(Ce) altered to different degree by intergrown Th-bearing apatite/thorite assemblage. Fluid-involved reactions led to mineral transformations and redistribution of the elements like LREE, Y, Th, U, and formation of the inhomogeneous allanite-(Ce)/REE-epidote rims enveloping the aggregated earlier phases.

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