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Abstract
The new mineral zincorietveldite (IMA2022-070), Zn(UO
2
)(SO
4
)
2
(H
2
O)
5
, was found in the Blue Lizard mine, San Juan County, Utah, USA, where it occurs as yellow to orange–yellow blades in a secondary assemblage with bobcookite, coquimbite, halotrichite, libbyite, metavoltine, rhomboclase, römerite, tamarugite and voltaite. The streak is very pale yellow. Crystals are transparent with vitreous lustre. The tenacity is brittle, the Mohs hardness is ~2½ and the fracture is curved. Cleavage is excellent on {010}, good on {100} and fair on {001}. The mineral is easily soluble in H
2
O and has a calculated density of 3.376 g⋅cm
–3
. The mineral is optically biaxial (+) with α = 1.568(2), β = 1.577(2) and γ = 1.595(2); 2V = 70(1)°. Electron microprobe analyses provided (Zn
0.720
Mg
0.109
Fe
0.091
Mn
0.046
Co
0.035
)
Σ1.00
(UO
2
)(SO
4
)
2
(H
2
O)
5
. Zincorietveldite is orthorhombic,
Pmn
2
1
,
a
= 12.8712(9),
b
= 8.3148(4),
c
= 11.2959(4) Å,
V
= 1208.90(11) Å
3
and
Z
= 4. Zincorietveldite is the Zn analogue of rietveldite. The structural unit is a uranyl-sulfate chain that is also found in the structures of bobcookite, oldsite, oppenheimerite and svornostite.