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Foord, Eugene E., Cobban, Robert R., Brownfield, Isabelle K. (1985) Uranoan thorite in lithophysal rhyolite–Topaz Mountain, Utah, USA. Mineralogical Magazine, 49 (354) 729-731 doi:10.1180/minmag.1985.049.354.13

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Reference TypeJournal (article/letter/editorial)
TitleUranoan thorite in lithophysal rhyolite–Topaz Mountain, Utah, USA
JournalMineralogical MagazineISSN0026-461X
AuthorsFoord, Eugene E.Author
Cobban, Robert R.Author
Brownfield, Isabelle K.Author
Year1985 (December)Volume49
Page(s)729-731Issue354
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_49/49-354-729.pdf+
DOIdoi:10.1180/minmag.1985.049.354.13Search in ResearchGate
Mindat Ref. ID3793Long-form Identifiermindat:1:5:3793:2
GUIDfbf7f536-337b-40a1-8c76-e37b50389bf3
Full ReferenceFoord, Eugene E., Cobban, Robert R., Brownfield, Isabelle K. (1985) Uranoan thorite in lithophysal rhyolite–Topaz Mountain, Utah, USA. Mineralogical Magazine, 49 (354) 729-731 doi:10.1180/minmag.1985.049.354.13
Plain TextFoord, Eugene E., Cobban, Robert R., Brownfield, Isabelle K. (1985) Uranoan thorite in lithophysal rhyolite–Topaz Mountain, Utah, USA. Mineralogical Magazine, 49 (354) 729-731 doi:10.1180/minmag.1985.049.354.13
In(1985, December) Mineralogical Magazine Vol. 49 (354) Mineralogical Society
Abstract/NotesAbstractUranoan thorite crystals have been found occurring as a sparse constituent in lithophysae in 6.1 to 6.8 Ma alkali rhyolite flows at Thomas Mountain, Utah, USA. The crystals are associated with sandidine, quartz, topaz, hematite, magnetite, and calcite; they are leek to dark grass green, transparent, well-formed, euhedral prisms, showing development of forms {100}, {101}, and {111}. The mineral is both optically isotropic, with a refractive index of 1.86(1), and X-ray amorphous, indicating its metamict state. Electron microprobe analysis yields: SiO2 17.3, ThO2 56.8, UO2 25.4, total 99.5%, and a structural formula of (Th0.72U0.31)Σ1.03Si0.97O4.This appears to be the first reported occurrence of thorite in volcanic rocks of rhyolitic composition, and may account for part or all of the Th reported in alkali rhyolites and so-called ‘topaz-rhyolites’ of the western USA.


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