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Yao, Wei, Liu, Peng, Li, Guowu, Sun, Ningyue, Yang, Wenqiang, Jiang, Chengyao, Du, Wei, Zhang, Chao, Song, Wenlei, Cook, Nigel J., Mao, and Jingwen (2024) Yuchuanite-(Y), Y2(CO3)3·H2O, a new hydrous yttrium carbonate mineral from the Yushui Cu deposit, South China. American Mineralogist, 109 (3) 599-605

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Reference TypeJournal (article/letter/editorial)
TitleYuchuanite-(Y), Y2(CO3)3·H2O, a new hydrous yttrium carbonate mineral from the Yushui Cu deposit, South China.
JournalAmerican Mineralogist
AuthorsYao, WeiAuthor
Liu, PengAuthor
Li, GuowuAuthor
Sun, NingyueAuthor
Yang, WenqiangAuthor
Jiang, ChengyaoAuthor
Du, WeiAuthor
Zhang, ChaoAuthor
Song, WenleiAuthor
Cook, Nigel J.Author
Mao, and JingwenAuthor
Year2024 (March)Volume<   109   >
Issue<   3   >
Original EntryWei Yao, Peng Liu, Guowu Li, Ningyue Sun, Wenqiang Yang, Chengyao Jiang, Wei Du, Chao Zhang, Wenlei Song, Nigel J. Cook, and Jingwen Mao (2023) Yuchuanite-(Y), Y2(CO3)3·H2O, a new hydrous yttrium carbonate mineral from the Yushui Cu deposit, South China. American Mineralogist, in press.
Classification
Not set
LoC
Not set
Mindat Ref. ID16143784Long-form Identifiermindat:1:5:16143784:8
GUID0
Full ReferenceYao, Wei, Liu, Peng, Li, Guowu, Sun, Ningyue, Yang, Wenqiang, Jiang, Chengyao, Du, Wei, Zhang, Chao, Song, Wenlei, Cook, Nigel J., Mao, and Jingwen (2024) Yuchuanite-(Y), Y2(CO3)3·H2O, a new hydrous yttrium carbonate mineral from the Yushui Cu deposit, South China. American Mineralogist, 109 (3) 599-605
Plain TextYao, Wei, Liu, Peng, Li, Guowu, Sun, Ningyue, Yang, Wenqiang, Jiang, Chengyao, Du, Wei, Zhang, Chao, Song, Wenlei, Cook, Nigel J., Mao, and Jingwen (2024) Yuchuanite-(Y), Y2(CO3)3·H2O, a new hydrous yttrium carbonate mineral from the Yushui Cu deposit, South China. American Mineralogist, 109 (3) 599-605
InLink this record to the correct parent record (if possible)
Abstract/NotesA new mineral species, yuchuanite-(Y), ideally Y2(CO3)3·H2O, has been discovered and characterized in the Yushui Cu deposit in South China. The mineral occurs in bedded/massive ore and is
associated with bornite, chalcopyrite, galena, sphalerite, bastnäsite-(Y), xenotime-(Y), anhydrite, and
quartz. Individual crystals range in size from 30 to 300 μm. No twinning is observed. The mineral
is colorless and transparent with a vitreous luster. The calculated density is 3.62 g/cm3
. An electron
microprobe analysis yields the empirical formula (based on 10 O apfu), (Y1.61Yb0.11Er0.11Dy0.08Ho0.03
Gd0.02Tm0.02)Σ1.99(CO3)3·H2O.
Yuchuanite-(Y) is triclinic, with space group P1 (#2), Z = 6, and unit-cell parameters a =
6.2134(3) Å, b = 8.9697(3) Å, c = 19.9045(7) Å, α = 91.062(3)°, β = 90.398(3)°, γ = 91.832(3)°, and
V = 1108.54(8) Å3
. The structure is constructed from (110) sheets of eight-coordinated Y polyhedra
and C trigonal planar groups. All Y polyhedra are linked by shared edges. The Y atoms occupy six
independent crystallographic sites of two different coordination types: [YO7(H2O)] and [YO8].
The chemical composition of yuchuanite-(Y) is similar to tengerite-(Y), Y2(CO3)3·2–3H2O, but
is distinct in the crystal structure, such as crystal system, space group, and unit cell, from that of
tengerite-(Y). The Y polyhedra of tengerite-(Y) are nine-coordinated, while those of yuchuanite-(Y)
are eight-coordinated. Moreover, their structures could be both described as sheet structures built up
from Y polyhedra and CO3 trigonal planar groups but link together in significantly different ways. Thus,
yuchuanite-(Y) is not a polytype of tengerite-(Y) but is an independent mineral species.

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Yuchuanite-(Y)


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