Thorianite

 Thorianite is a rare thorium oxide mineral, ThO2.[4] It was originally described by Ananda Coomaraswamy in 1904 as uraninite,[5] but recognized as a new species by Wyndham R. Dunstan.[6] It was so named by Dunstan on account of its high percentage of thorium; it also contains the oxides of uranium, lanthanum, cerium, praseodymium and neodymium. Helium is present, and the mineral is slightly less radioactive than pitchblende,[7] but is harder to shield due to its high energy gamma rays. It is common in the alluvial gem-gravels of Sri 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 from Madagascar.

Thorianite
Thorianite-54888.jpg
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
Strunz classification4.DL.05
Crystal systemIsometric
Crystal classHexoctahedral (m3m)
H-M symbol: (4/m 3 2/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 scale hardness6.5 – 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.svg Radioactive
References[1][2][3]

ChemistryEdit

Based on color, specific gravity and composition three types of thorianite are distinguished:[8]

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

Thorianite and uraninite form a complete solid solution series in synthetic and natural material.[9] 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%.[10] Rare earths, chiefly Ce, substitute for Th in amounts up to 8% by weight.[9][11] 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.

VarietiesEdit

  • Aldanite – a variety of thorianite containing 14.9% to 29.0% UO2 and 11.2% to 12.5% PbO.[12]
  • Uranothorianite[13]
  • Thorianite Cerian[14][15]
  • Thorianite La bearing[14]

OccurrenceEdit

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

  • Sri Lanka – In stream gravels, Galle district, Southern Province; Balangoda district; near KodrugalaSabaragamuwa Province; and from a pegmatite in Bambarabotuwa area.
  • India – Reported from beach sands of Travancore (Kerala).[16]
  • Madagascar – Found in alluvial deposits of Betroka and Andolobe.[17] Also as very large crystals from Tôlanaro (Fort Dauphin); at Andranondambo and other localities.
  • Russia – In black sands of a gold placer on Boshogoch RiverTransbaikaliaSiberia; in the Kovdor Massif by KovdorKola Peninsula; in the Yenisei Range, Siberia.
  • United States – reported from EastonPennsylvania; black sands in Missouri River, near HelenaMontanaScott RiverSiskiyou CountyCalifornia;[18] black sands in Nixon Fork and Wiseman districts, Alaska.[19][20]
  • Canada – Reported with uraninite in a pegmatite on Charlebois Lake, east of Lake Athabasca;[21] Uranon variety reported from pegmatite and metesomatized zones in crystalline limestones from many locations in Quebec and Ontario.[22]
  • South Africa – Occurs with baddeleyite as an accessory in carbonatite at PhalaborwaEastern Transvaal.[23]
  • Democratic Republic of Congo - Kasaï region

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 Metasyntactic variable, which is released under the 
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