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Xue, Yuan, Sun, Ningyue, He, Hongping, Chen, Aiqing, Yang, Yiping (2022) Liguowuite, WO3, a new member of the A-site vacant perovskite type minerals from the Panzhihua–Xichang region, China. European Journal of Mineralogy, 34 (1) 95-108 doi:10.5194/ejm-34-95-2022

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Reference TypeJournal (article/letter/editorial)
TitleLiguowuite, WO3, a new member of the A-site vacant perovskite type minerals from the Panzhihua–Xichang region, China
JournalEuropean Journal of MineralogyISSN0935-1221
AuthorsXue, YuanAuthor
Sun, NingyueAuthor
He, HongpingAuthor
Chen, AiqingAuthor
Yang, YipingAuthor
Year2022 (February 8)Volume34
Page(s)95-108Issue1
PublisherCopernicus GmbH
URL
Download URLhttps://ejm.copernicus.org/articles/34/95/2022/ejm-34-95-2022.pdf+
DOIdoi:10.5194/ejm-34-95-2022Search in ResearchGate
Classification
Not set
LoC
Not set
Mindat Ref. ID17068367Long-form Identifiermindat:1:5:17068367:0
GUID58407c1e-3b50-40f4-bb8b-2ad6482b56d3
Full ReferenceXue, Yuan, Sun, Ningyue, He, Hongping, Chen, Aiqing, Yang, Yiping (2022) Liguowuite, WO3, a new member of the A-site vacant perovskite type minerals from the Panzhihua–Xichang region, China. European Journal of Mineralogy, 34 (1) 95-108 doi:10.5194/ejm-34-95-2022
Plain TextXue, Yuan, Sun, Ningyue, He, Hongping, Chen, Aiqing, Yang, Yiping (2022) Liguowuite, WO3, a new member of the A-site vacant perovskite type minerals from the Panzhihua–Xichang region, China. European Journal of Mineralogy, 34 (1) 95-108 doi:10.5194/ejm-34-95-2022
In(2022) European Journal of Mineralogy Vol. 34 (1) Schweizerbart
Abstract/NotesA new member of the non-stoichiometric perovskite group mineral species, liguowuite, ideally WO3, has been found in the Neoproterozoic Sinian biotite-quartz monzonite in the southern part of the Panzhihua–Xichang region (Nanyang village: 26∘46′8.21′′ N, 101∘27′13.86′′ E), China. It is associated with hornblende, pargasite, ferro-hornblende, annite, hydrobiotite, phlogopite, orthoclase, microcline, albite, quartz, kaolinite, ilmenite, goethite, hematite, magnetite, pyrite, zircon, zoisite, titanite, epidote, diopside, tourmaline, almandine, fluorapatite, monazite-(Ce), allanite-(Ce), bastnäsite-(Ce), xenotime-(Y), scheelite, moissanite, tellurite, wumuite, and tewite. Liguowuite occurs as greenish yellow prisms, ranging from 0.05 to 0.1 mm in diameter, and it is transparent with a greasy luster and a white streak. Liguowuite exhibits a triclinic pseudomorphism composed of nanoparticles with many cracks and nanovoids. This mineral is brittle and has a Mohs hardness value of approximately 3–4. The calculated density is 7.22 g cm−3. Electron microprobe analyses gave (average weight percent, wt %, of 15 spot analyses of 4 samples) K2O = 0.01, WO3 = 99.23, TeO2 = 0.03, CaO = 0.06, Na2O = 0.04, and total 99.37, yielding the empirical formula W1.00O3, based on Oapfu=3 and ideally WO3. The strongest five diffraction lines (d Å (I)(hkl)) are 3.8552 (88)(002), 3.7685 (88)(020), 3.6590 (100)(–200), 2.6928 (43)(022), and 2.6258 (60)(202). Liguowuite is monoclinic and is in space group P21/n, with a= 7.32582(18) Å, b= 7.54767(18) Å, c= 7.71128(18) Å, β= 90.678(3)∘, V= 426.348(19) Å3, and Z= 8. The crystal structure data were refined using the Rietveld refinement method and X-ray powder diffraction data. The reliability factors (R factors) were Rwp= 0.0604 and Rp= 0.0454, with χ2 = 1.707. Liguowuite consists of corner-sharing distorted and tilted [WO6] octahedra, in which the W atoms are off-center and form six W–O bonds ranging from 1.7 to 2.2 Å with the surrounding oxygen atoms. According to the hierarchical scheme for perovskite supergroup minerals, liguowuite is the first reported example of A-site vacant single oxide, i.e., a new perovskite subgroup.

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Map of Localities

Locality Pages

LocalityCitation Details
Nanyang, Huaping County, Lijiang, Yunnan, China

Mineral Pages

MineralCitation Details
Liguowuite
Liguowuite Subgroup

Mineral Occurrences

LocalityMineral(s)
Nanyang, Huaping County, Lijiang, Yunnan, China Almandine, Annite, Bastnäsite-(Ce), Diopside, Epidote, Ferro-hornblende, Fluorapatite, Hydrobiotite, Liguowuite, Magnetite, Microcline, Moissanite, Pargasite, Phlogopite, Pyrite, Titanite, Xenotime-(Y)


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