thorianite

{{Infobox mineral

|boxbgcolor=#6d625d| name = Thorianite

| boxtextcolor = #fff

| category = Oxide mineral

| image = Thorianite-54888.jpg

| caption = Group of interpenetrating twinned thorianite crystals from Ambatofotsy, Madagascar (size: 1.6 x 1.4 x 1.3 cm)

| formula = Thorium oxide, ThO2

| IMAsymbol = Tho{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}

| molweight =

| strunz = 4.DL.05

| system = Isometric

| class = Hexoctahedral (m{{overline|3}}m)
H-M symbol: (4/m {{overline|3}} 2/m)

| symmetry = Fm3m

| unit cell = a = 5.595 Å; Z = 4

| color = Dark gray, brown-black

| 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 = 6.5 – 7

| luster = Resinous, sub-metallic

| refractive = n = 2.20 – 2.35

| opticalprop = Isotropic

| birefringence =

| pleochroism =

| streak = Grey, grey green to black

| gravity = 9.7

| density =

| melt =

| fusibility =

| diagnostic =

| solubility =

| diaphaneity = Opaque, translucent on thin edges

| other = 25px Radioactive

| references = {{Cite web |url=http://www.handbookofmineralogy.com/pdfs/thorianite.pdf |title=Handbook of Mineralogy |access-date=2011-12-10 |archive-date=2016-03-03 |archive-url=https://web.archive.org/web/20160303170830/http://www.handbookofmineralogy.com/pdfs/thorianite.pdf |url-status=dead }}[http://www.mindat.org/min-3944.html Mindat.org][http://www.webmineral.com/data/Thorianite.shtml Webmineral data]

}}

Thorianite is a rare thorium oxide mineral, ThO2.{{Cite book

| publisher = United States Government Printing Office

| last = Frondel

| first = C.

| title = Systematic Mineralogy of Uranium and Thorium

| year = 1958

}} It was originally described by Ananda Coomaraswamy in 1904 as uraninite,{{Cite journal

| volume = Pt. 6

| issue = 2

| pages = 57

| last = Coomaraswamy

| first = A.K.

| title = Uraninite

| journal = Spolia Zeylanica

| year = 1904

}} but recognized as a new species by Wyndham R. Dunstan.{{Cite journal

| volume = 69

| pages = 510–511

| last = Dunstan

| first = Wyndham R.

| title = The occurrence of Thorium in Ceylon

| journal = Nature

| date = 1904-03-31

| doi = 10.1038/069510d0

| issue=1796

|bibcode = 1904Natur..69..510D | s2cid = 4032255

| url = https://zenodo.org/record/1429437

}} 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,{{EB1911|inline=y|wstitle=Thorianite|volume=26|page=878}} 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 {{convert|6|cm|abbr=on}}, have been reported from Madagascar.

Chemistry

Based on color, specific gravity and composition three types of thorianite are distinguished:{{Cite journal

| volume = 1

| issue = Ist Ser

| pages = 201–206

| last = Kobayashi

| first = M.

| title = On the composition of thorianite

| journal = Tohoku Imp. Univ. Sci. Repts.

| year = 1912

}}

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

Thorianite and uraninite form a complete solid solution series in synthetic and natural material.{{Cite book

| pages = 620–622

| last = Palache

| first = C.

|author2=H. Berman |author3=C. Frondel

| title = Dana's System of Mineralogy, Volume 1

| publisher = John Wiley and Sons, New York

| year = 1944

}} The division between the two species is at Th:U = 1:1 with uranium possibly making up to 46.50% and thorium ranging up to 87.88%.

{{Cite book

| publisher = McGraw-Hill

| last = Heinrich

| first = E. W.

| title = Mineralogy and Geology of Radioactive Raw Materials

| year = 1958

}} Rare earths, chiefly cerium, substitute for thorium in amounts up to 8% by mass.{{Cite journal

| volume = 40

| last = Graham

| first = A. R.

| title = CERIANITE CeO2: A NEW RARE-EARTH OXIDE MINERAL

| journal = Am. Mineral.

| year = 1955

}} Cerium is probably present as Ce4+. Complete series is known in synthetic material between CeO2 - PrO2 - ThO2 - UO2. Small amounts of Fe3+ and zirconium also may be isomorphous with thorium. Lead present is probably radiogenic.

Varieties

  • Aldanite – a variety of thorianite containing 14.9% to 29.0% UO2 and 11.2% to 12.5% PbO.{{Cite journal

| volume = II

| issue = 6

| pages = 105–107

| last = Bespalov

| first = M.M.

| title = On discovery of a new mineral of the thorianite group [in Russian]

| journal = Sovietskaya Geologiya

| year = 1941

}}

  • Uranothorianite{{Cite web

| title = Uranothorianite mineral information and data

| accessdate = 2007-06-28

| url = http://www.mindat.org/min-4114.html

}}

  • Thorianite Cerian{{Cite web

|title = Minerals with crystal structure determined

|accessdate = 2007-06-27

|url = http://sdpd.univ-lemans.fr/minknown.html#T

|url-status = dead

|archiveurl = https://web.archive.org/web/20070927022021/http://sdpd.univ-lemans.fr/minknown.html#T

|archivedate = 2007-09-27

}}{{Cite web

|title = ICSD for WWW : Details (Thorianite Cerian)

|accessdate = 2007-06-27

|url = http://icsdweb.fiz-karlsruhe.de/details.php?id%5B%5D=24439&PHPSESSID=734118bb8

}}{{Dead link|date=June 2018 |bot=InternetArchiveBot |fix-attempted=no }}

  • Thorianite La bearing

Occurrence

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

| volume = 88

| pages = 282

| last = Viswanathan

| first = P.

| title = Thorianite in Travancore

| journal = Mineral. Mag.

| year = 1953

}}

| publisher = Augustin Challamel, éditeur, Librairie maritime et coloniale

| last = Lacroix

| first = A.

| title = Minéralogie de Madagascar

| url = https://archive.org/details/MineralogieDeMadagascarTome3

| year = 1923

}} Also as very large crystals from Fort Dauphin; at Andranondambo and other localities.

| pages = 198

| last = George

| first = D'Arcy

| title = Mineralogy of Uranium and Thorium Bearing Minerals

| journal = USAEC Technical Information Service, Oak Ridge, Tennessee

| series = RMO-563

| year = 1949

}} black sands in Nixon Fork and Wiseman districts, Alaska.{{Cite book

| publisher = GS-C-195, Geological Survey

| last = White

| first = M. G.

| title = Radioactivity of Selected Rocks and Placer Concentrates from Northeastern Alaska

| year = 1952

}}{{Cite journal

| publisher = TEI-192, Geological Survey

| last = White

| first = M. G.

|author2=J. M. Stevens

| title = Reconnaissance For Radioactive Deposits In The Ruby-Poorman District, Ruby Quadrangle, Central Alaska,1949

| journal = USGS Report

| year = 1953

| page = 62

| doi = 10.3133/tei192

| bibcode = 1953usgs.rept...62W

| url = https://digital.library.unt.edu/ark:/67531/metadc1050378/m2/1/high_res_d/report.pdf

}}

| publisher = Geological Survey of Canada

| last = Lang

| first = A. H.

|author2=J. W. Griffith |author3=H. R. Steacy

| title = Canadian Deposits of Uranium and Thorium

| year = 1962

}} Uranon variety reported from pegmatite and metesomatized zones in crystalline limestones from many locations in Quebec and Ontario.{{Cite journal

| volume = 40

| last = Robinson

| first = S. C.

|author2=A. P. Sabina

| title = Uraninite And Thorianite From Ontario And Quebec

| journal = Am. Mineral.

| year = 1955

}}

| volume = 40

| pages = 275–282

| last = Hiemstra

| first = S. A.

| title = Baddeleyite from Phalaborwa, Eastern Transvaal

| journal = American Mineralogist

| year = 1955

}}

| volume = 40

| pages = C177

| last = Ledoux

| first = A.

| title = Les roches cristallines du Kasai

| journal = Soc. Geol. Belgique Annales

}}

See also

References

{{reflist | 2}}