Monazite-(Gd), a new Gd-dominant mineral of the monazite group from the Zimná Voda REE–U–Au quartz vein, Prakovce, Western Carpathians, Slovakia
Monazite-(Gd), ideally GdPO 4 , is a new mineral of the monazite group. It was discovered near Prakovce-Zimná Voda, ~23 km WNW of Košice, Western Carpathians, Slovakia. It forms anhedral domains (≤100 μm, mostly 10–50 μm in size), in close association with monazite-(Sm), Gd-bearing xenotime-(Y), Gd-...
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Veröffentlicht in: | Mineralogical magazine 2023-08, Vol.87 (4), p.568-574 |
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Sprache: | eng |
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Zusammenfassung: | Monazite-(Gd), ideally GdPO
4
, is a new mineral of the monazite group. It was discovered near Prakovce-Zimná Voda, ~23 km WNW of Košice, Western Carpathians, Slovakia. It forms anhedral domains (≤100 μm, mostly 10–50 μm in size), in close association with monazite-(Sm), Gd-bearing xenotime-(Y), Gd-bearing hingganite-(Y), fluorapatite and uraninite. All these minerals are hosted in a REE–U–Au quartz–muscovite vein, hosted in phyllites in an exocontact to granites. The density calculated using the average empirical formula and unit-cell parameters is 5.55 g/cm
3
. The average chemical composition measured by means of electron microprobe is as follows (wt.%): P
2
O
5
29.68, As
2
O
5
0.15, SiO
2
0.07, ThO
2
0.01, UO
2
0.04, Y
2
O
3
1.30, La
2
O
3
3.19, Ce
2
O
3
6.93, Pr
2
O
3
1.12, Nd
2
O
3
10.56, Sm
2
O
3
17.36, Eu
2
O
3
1.49, Gd
2
O
3
22.84, Tb
2
O
3
1.57, Dy
2
O
3
2.27, CaO 0.21, total 99.67. The corresponding empirical formula calculated on the basis of 4 oxygen atoms is: (Gd
0.30
Sm
0.24
Nd
0.15
Ce
0.10
La
0.05
Dy
0.03
Y
0.03
Tb
0.02
Eu
0.02
Pr
0.02
Ca
0.01
)
0.98
P
1.01
O
4
. The ideal formula is GdPO
4
. The monazite-type structure has been confirmed by micro-Raman spectroscopy and selected-area electron diffraction. Monazite-(Gd) is monoclinic, space group
P
2
1
/
n
,
a
= 6.703(1) Å,
b
= 6.914(1) Å,
c
= 6.383(1) Å, β = 103.8(1)°,
V
= 287.3(1) Å
3
and Z = 4. The middle REE enrichment of monazite-(Gd) is shared with the associated Gd-bearing xenotime-(Y) to ‘xenotime-(Gd)’ and Gd-bearing hingganite-(Y). This exotic REE signature and precipitation of Gd-bearing mineral assemblage is a product of selective complexing and enrichment in middle REE in low-temperature hydrothermal fluids by alteration of primary uraninite, brannerite and fluorapatite on a micro-scale. The new mineral is named as an analogue of monazite-(La), monazite-(Ce), monazite-(Nd) and monazite-(Sm) but with Gd dominant among the REE. |
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ISSN: | 0026-461X 1471-8022 |
DOI: | 10.1180/mgm.2023.37 |