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 | |
---|---|
General | |
Category | Oxide mineral |
Formula (repeating unit) | Thorium oxide,ThO2 |
IMA symbol | Tho[1] |
Strunz classification | 4.DL.05 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol:(4/m32/m) |
Space group | Fm3m |
Unit cell | a = 5.595 Å; Z = 4 |
Identification | |
Color | Dark gray, brown-black |
Crystal habit | Cubic crystals, usually rounded to some degree in detrital deposits |
Twinning | Penetration twins on {111} common |
Cleavage | Poor/Indistinct |
Fracture | Irregular to uneven, sub-conchoidal |
Mohs scalehardness | 6.5 – 7 |
Luster | Resinous, sub-metallic |
Streak | Grey, grey green to black |
Diaphaneity | Opaque, translucent on thin edges |
Specific gravity | 9.7 |
Optical properties | Isotropic |
Refractive index | n = 2.20 – 2.35 |
Other characteristics | Radioactive |
References | [2][3][4] |
Chemistry
editBased 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
editOccurrence
editUsually found in alluvial deposits, beach sands, heavy mineral placers, andpegmatites.
- Sri Lanka – In stream gravels,Galledistrict, Southern Province;Balangodadistrict; nearKodrugala,SabaragamuwaProvince; and from a pegmatite inBambarabotuwaarea.
- India– Reported from beach sands ofTravancore(Kerala).[17]
- Madagascar– Found in alluvial deposits ofBetrokaandAndolobe.[18]Also as very large crystals fromFort Dauphin;atAndranondamboand other localities.
- Russia– In black sands of a gold placer onBoshogoch River,Transbaikalia,Siberia;in theKovdor MassifbyKovdor,Kola Peninsula;in theYenisei Range,Siberia.
- United States– reported fromEaston,Pennsylvania;black sands inMissouri River,nearHelena,Montana;Scott River,Siskiyou County,California;[19]black sands inNixon ForkandWisemandistricts,Alaska.[20][21]
- Canada– Reported with uraninite in a pegmatite onCharlebois Lake,east ofLake Athabasca;[22]Uranon variety reported frompegmatiteand metesomatized zones in crystalline limestones from many locations inQuebecandOntario.[23]
- South Africa– Occurs withbaddeleyiteas an accessory incarbonatiteatPhalaborwa,Eastern Transvaal.[24]
- Democratic Republic of Congo-Kasaï region[25]
See also
editReferences
edit- ^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.
- ^"Handbook of Mineralogy"(PDF).Archived fromthe original(PDF)on 2016-03-03.Retrieved2011-12-10.
- ^Mindat.org
- ^Webmineral data
- ^Frondel, C. (1958).Systematic Mineralogy of Uranium and Thorium.United States Government Printing Office.
- ^Coomaraswamy, A.K. (1904). "Uraninite".Spolia Zeylanica.Pt. 6 (2): 57.
- ^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.
- ^public domain:Chisholm, Hugh,ed. (1911). "Thorianite".Encyclopædia Britannica.Vol. 26 (11th ed.). Cambridge University Press. p. 878. One or more of the preceding sentences incorporates text from a publication now in the
- ^Kobayashi, M. (1912). "On the composition of thorianite".Tohoku Imp. Univ. Sci. Repts.1(Ist Ser): 201–206.
- ^abPalache, C.; H. Berman; C. Frondel (1944).Dana's System of Mineralogy, Volume 1.John Wiley and Sons, New York. pp. 620–622.
- ^ Heinrich, E. W. (1958).Mineralogy and Geology of Radioactive Raw Materials.McGraw-Hill.
- ^Graham, A. R. (1955). "CERIANITE CeO2:A NEW RARE-EARTH OXIDE MINERAL ".Am. Mineral.40.
- ^Bespalov, M.M. (1941). "On discovery of a new mineral of the thorianite group [in Russian]".Sovietskaya Geologiya.II(6): 105–107.
- ^"Uranothorianite mineral information and data".Retrieved2007-06-28.
- ^ab"Minerals with crystal structure determined".Archived fromthe originalon 2007-09-27.Retrieved2007-06-27.
- ^"ICSD for WWW: Details (Thorianite Cerian)".Retrieved2007-06-27.[permanent dead link ]
- ^Viswanathan, P. (1953). "Thorianite in Travancore".Mineral. Mag.88:282.
- ^Lacroix, A. (1923).Minéralogie de Madagascar.Augustin Challamel, éditeur, Librairie maritime et coloniale.
- ^George, D'Arcy (1949). "Mineralogy of Uranium and Thorium Bearing Minerals".USAEC Technical Information Service, Oak Ridge, Tennessee.RMO-563: 198.
- ^White, M. G. (1952).Radioactivity of Selected Rocks and Placer Concentrates from Northeastern Alaska.GS-C-195, Geological Survey.
- ^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.
- ^Lang, A. H.; J. W. Griffith; H. R. Steacy (1962).Canadian Deposits of Uranium and Thorium.Geological Survey of Canada.
- ^Robinson, S. C.; A. P. Sabina (1955). "Uraninite And Thorianite From Ontario And Quebec".Am. Mineral.40.
- ^Hiemstra, S. A. (1955). "Baddeleyite from Phalaborwa, Eastern Transvaal".American Mineralogist.40:275–282.
- ^Ledoux, A. "Les roches cristallines du Kasai".Soc. Geol. Belgique Annales.40:C177.