Thorianiteis a rarethoriumoxide mineral,ThO2.[5]It was originally described byAnanda Coomaraswamyin 1904 as uraninite,[6]but recognized as a new species byWyndham R. Dunstan.[7]It was so named by Dunstan on account of its high percentage ofthorium;it also contains the oxides ofuranium,lanthanum,cerium,praseodymiumandneodymium.Heliumis present, and the mineral is slightly lessradioactivethanpitchblende,[8]but is harder to shield due to its high energy gamma rays. It is common in thealluvialgem-gravels ofSri Lanka,where it occurs mostly as water worn, small, heavy, black, cubic crystals. The largest crystals are usually near 1.5 cm. Larger crystals, up to 6 cm (2.4 in), have been reported fromMadagascar.

Thorianite
Group of interpenetrating twinned thorianite crystals from Ambatofotsy, Madagascar (size: 1.6 x 1.4 x 1.3 cm)
General
CategoryOxide mineral
Formula
(repeating unit)
Thorium oxide,ThO2
IMA symbolTho[1]
Strunz classification4.DL.05
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H-M symbol:(4/m32/m)
Space groupFm3m
Unit cella = 5.595 Å; Z = 4
Identification
ColorDark gray, brown-black
Crystal habitCubic crystals, usually rounded to some degree in detrital deposits
TwinningPenetration twins on {111} common
CleavagePoor/Indistinct
FractureIrregular to uneven, sub-conchoidal
Mohs scalehardness6.5 – 7
LusterResinous, sub-metallic
StreakGrey, grey green to black
DiaphaneityOpaque, translucent on thin edges
Specific gravity9.7
Optical propertiesIsotropic
Refractive indexn = 2.20 – 2.35
Other characteristicsRadioactive
References[2][3][4]

Chemistry

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Based on color, specific gravity and composition three types of thorianite are distinguished:[9]

  • α-thorianite
  • β-thorianite
  • γ-thorianite

Thorianite anduraniniteform a completesolid solutionseries in synthetic and natural material.[10]The division between the two species is at Th:U = 1:1 with U possibly making up to 46.50% and Th ranging up to 87.88%.[11]Rare earths,chiefly Ce, substitute for Th in amounts up to 8% by weight.[10][12]Ce is probably present as Ce4+.Complete series is known in synthetic material between CeO2- PrO2- ThO2- UO2.Small amounts of Fe3+and Zr also may be isomorphous with Th. Pb present is probably radiogenic.

Varieties

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  • Aldanite– a variety of thorianite containing 14.9% to 29.0% UO2and 11.2% to 12.5% PbO.[13]
  • Uranothorianite[14]
  • Thorianite Cerian[15][16]
  • Thorianite La bearing[15]

Occurrence

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Usually found in alluvial deposits, beach sands, heavy mineral placers, andpegmatites.

See also

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References

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  1. ^Warr, L.N. (2021)."IMA–CNMNC approved mineral symbols".Mineralogical Magazine.85(3): 291–320.Bibcode:2021MinM...85..291W.doi:10.1180/mgm.2021.43.S2CID235729616.
  2. ^"Handbook of Mineralogy"(PDF).Archived fromthe original(PDF)on 2016-03-03.Retrieved2011-12-10.
  3. ^Mindat.org
  4. ^Webmineral data
  5. ^Frondel, C. (1958).Systematic Mineralogy of Uranium and Thorium.United States Government Printing Office.
  6. ^Coomaraswamy, A.K. (1904). "Uraninite".Spolia Zeylanica.Pt. 6 (2): 57.
  7. ^Dunstan, Wyndham R. (1904-03-31)."The occurrence of Thorium in Ceylon".Nature.69(1796): 510–511.Bibcode:1904Natur..69..510D.doi:10.1038/069510d0.S2CID4032255.
  8. ^One or more of the preceding sentences incorporates text from a publication now in thepublic domain:Chisholm, Hugh,ed. (1911). "Thorianite".Encyclopædia Britannica.Vol. 26 (11th ed.). Cambridge University Press. p. 878.
  9. ^Kobayashi, M. (1912). "On the composition of thorianite".Tohoku Imp. Univ. Sci. Repts.1(Ist Ser): 201–206.
  10. ^abPalache, C.; H. Berman; C. Frondel (1944).Dana's System of Mineralogy, Volume 1.John Wiley and Sons, New York. pp. 620–622.
  11. ^ Heinrich, E. W. (1958).Mineralogy and Geology of Radioactive Raw Materials.McGraw-Hill.
  12. ^Graham, A. R. (1955). "CERIANITE CeO2:A NEW RARE-EARTH OXIDE MINERAL ".Am. Mineral.40.
  13. ^Bespalov, M.M. (1941). "On discovery of a new mineral of the thorianite group [in Russian]".Sovietskaya Geologiya.II(6): 105–107.
  14. ^"Uranothorianite mineral information and data".Retrieved2007-06-28.
  15. ^ab"Minerals with crystal structure determined".Archived fromthe originalon 2007-09-27.Retrieved2007-06-27.
  16. ^"ICSD for WWW: Details (Thorianite Cerian)".Retrieved2007-06-27.[permanent dead link]
  17. ^Viswanathan, P. (1953). "Thorianite in Travancore".Mineral. Mag.88:282.
  18. ^Lacroix, A. (1923).Minéralogie de Madagascar.Augustin Challamel, éditeur, Librairie maritime et coloniale.
  19. ^George, D'Arcy (1949). "Mineralogy of Uranium and Thorium Bearing Minerals".USAEC Technical Information Service, Oak Ridge, Tennessee.RMO-563: 198.
  20. ^White, M. G. (1952).Radioactivity of Selected Rocks and Placer Concentrates from Northeastern Alaska.GS-C-195, Geological Survey.
  21. ^White, M. G.; J. M. Stevens (1953). "Reconnaissance For Radioactive Deposits In The Ruby-Poorman District, Ruby Quadrangle, Central Alaska,1949".USGS Report.TEI-192, Geological Survey: 62.Bibcode:1953usgs.rept...62W.doi:10.3133/tei192.
  22. ^Lang, A. H.; J. W. Griffith; H. R. Steacy (1962).Canadian Deposits of Uranium and Thorium.Geological Survey of Canada.
  23. ^Robinson, S. C.; A. P. Sabina (1955). "Uraninite And Thorianite From Ontario And Quebec".Am. Mineral.40.
  24. ^Hiemstra, S. A. (1955). "Baddeleyite from Phalaborwa, Eastern Transvaal".American Mineralogist.40:275–282.
  25. ^Ledoux, A. "Les roches cristallines du Kasai".Soc. Geol. Belgique Annales.40:C177.
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