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Kampf, Anthony R., Ma, Chi, Marty, Joe (2023) Chinleite-(Nd), NaNd(SO4)2(H2O), the Nd analogue of chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA. The Canadian Journal of Mineralogy and Petrology, 61 (2) 411-418 doi:10.3749/2200065

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Reference TypeJournal (article/letter/editorial)
TitleChinleite-(Nd), NaNd(SO4)2(H2O), the Nd analogue of chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA
JournalThe Canadian Journal of Mineralogy and Petrology
AuthorsKampf, Anthony R.Author
Ma, ChiAuthor
Marty, JoeAuthor
Year2023Volume61
Page(s)411-418Issue2
PublisherGeoScienceWorld
DOIdoi:https://doi.org/10.3749/2200065Search in ResearchGate
Original EntryKampf, A.R., Ma, C., Marty, J.R. (2023): Chinleite-(Nd), NaNd(SO4)2(H2O), the analogue of chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA. The Canadian Journal of Mineralogy and Petrology: 61 (in press).
Classification
Not set
LoC
Not set
Mindat Ref. ID16143682Long-form Identifiermindat:1:5:16143682:7
GUIDa5b1571e-8d97-49d7-baea-1233c658f9ed
Full ReferenceKampf, Anthony R., Ma, Chi, Marty, Joe (2023) Chinleite-(Nd), NaNd(SO4)2(H2O), the Nd analogue of chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA. The Canadian Journal of Mineralogy and Petrology, 61 (2) 411-418 doi:10.3749/2200065
Plain TextKampf, Anthony R., Ma, Chi, Marty, Joe (2023) Chinleite-(Nd), NaNd(SO4)2(H2O), the Nd analogue of chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA. The Canadian Journal of Mineralogy and Petrology, 61 (2) 411-418 doi:10.3749/2200065
In(2023) The Canadian Journal of Mineralogy and Petrology Vol. 61 (2) Mineralogical Association of Canada
Abstract/NotesChinleite-(Nd) (IMA2022-051), NaNd(SO4)2(H2O), is a new mineral discovered in efflorescence on tunnel walls in the Markey mine, Red Canyon, White Canyon district, San Juan County, Utah, USA. It occurs as colorless prisms with pyramidal terminations in association with gypsum and natrozippeite on asphaltite. Crystals are transparent with vitreous luster. The mineral has a white streak, Mohs hardness 2½–3, one good cleavage (probably on {100}), brittle tenacity, and a splintery fracture. The calculated density is 3.436 g/cm3. Electron probe microanalysis provided the empirical formula (Ca0.538Na0.395Nd0.244Sm0.150Ce0.130Y0.117Gd0.113Dy0.061Pr0.043Sr0.032Eu0.039La0.008Ho0.006)Σ1.876(SO4)2[(H2O)0.73(OH)0.27]. Chinleite-(Nd) is trigonal, P3221, a = 6.9540(7), c = 12.8590(9) Å, V = 538.52(11) Å3, and Z = 3. The structure of chinleite-(Nd) (R1 = 0.0258 for 791 I > 2σI reflections), a three-dimensional framework consisting of SO4 groups, irregular NaO8 polyhedra, and NdO9 distorted tri-capped trigonal prisms, is the same as that of chinleite-(Y) and similar to the structure of bassanite.

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Markey Mine, Red Canyon Mining District, San Juan County, Utah, USA

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Chinleite-(Nd)

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Markey Mine, Red Canyon Mining District, San Juan County, Utah, USA Chinleite-(Nd)


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