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Mannardite

A valid IMA mineral species
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About MannarditeHide

03682090017271925066904.jpg
George W. Mannard
Formula:
Ba(Ti4+6V3+2)O16
Formerly defined as BaxTi8-2xV2xO16·2-xH2O.
Colour:
Jet black
Lustre:
Adamantine
Hardness:
7
Specific Gravity:
4.12
Crystal System:
Tetragonal
Name:
The name honors Dr. George William Mannard (1932-1982), Canadian exploration geologist and mining executive, president of Kidd Creek Mines Ltd., for his long-standing interest in minerals and mineral deposits of British Columbia.
V analogue of redledgeite.

May stand for a vanadium ore in some black-schist deposits (Yang et al., 2023).


Unique IdentifiersHide

Mindat ID:
2567
Long-form identifier:
mindat:1:1:2567:2

Similar NamesHide

MahnertiteA valid IMA mineral speciesNaCu3(AsO4)2Cl · 5H2O
Monradite

IMA Classification of MannarditeHide

Approved
Approval year:
1983
First published:
1986

Classification of MannarditeHide

4.DK.05b

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
K : With large (+- medium-sized) cations; tunnel structures
7.9.5.1

7 : MULTIPLE OXIDES
9 : AB8X16
7.12.17

7 : Oxides and Hydroxides
12 : Oxides of V, Nb and Ta

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
ManIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of MannarditeHide

Adamantine
Transparency:
Opaque
Colour:
Jet black
Streak:
White to grayish-white
Hardness:
Tenacity:
Brittle
Cleavage:
Distinct/Good
Prominent {100} cleavage.
Fracture:
Irregular/Uneven, Sub-Conchoidal
Density:
4.12 g/cm3 (Measured)    4.28 g/cm3 (Calculated)
Comment:
Density of a Cr-free mannardite from Gacun Mine, Sichuan, China is 4.43 g/cm3; microindentation hardness measured on a sample coming from this locality is 609 Kg/mm2.

Optical Data of MannarditeHide

Type:
Uniaxial (+)
RI values:
nω = 2.26(1) nε = 2.42
Max. Birefringence:
δ = 0.160
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Anisotropism:
Strong; light pinkish-grey (Ro) to dark brownish-grey (Re).
Bireflectance:
Distinct; shades of light to dark brown.
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm16.5%18.0%
420nm16.3%17.6%
440nm16.0%17.2%
460nm15.7%17.0%
480nm15.5%16.9%
500nm15.4%17.0%
520nm15.2%17.2%
540nm15.1%17.4%
560nm15.0%17.7%
580nm15.0%17.9%
600nm15.0%18.1%
620nm15.0%18.3%
640nm15.0%18.4%
660nm15.0%18.5%
680nm15.1%18.6%
700nm15.1%18.6%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 18.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Pale reddish brown
Internal Reflections:
None

Chemistry of MannarditeHide

Mindat Formula:
Ba(Ti4+6V3+2)O16

Formerly defined as BaxTi8-2xV2xO16·2-xH2O.
Element Weights:
Element% weight
Ti36.708 %
O32.719 %
Ba17.552 %
V13.022 %

Calculated from ideal end-member formula.
Ti
O
Ba
V

Crystallography of MannarditeHide

Crystal System:
Tetragonal
Class (H-M):
4/m - Dipyramidal
Space Group:
I41/a
Cell Parameters:
a = 14.356 Å, c = 5.911 Å
Ratio:
a:c = 1 : 0.412
Unit Cell V:
1,218.23 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Prismatic, bounded by {110} and {001} (and rare {100}). Elongated along [001], flattened on {100}, bent or twisted about [001], deeply striated ‖ elongation. Also in fan-like aggregates.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0018319MannarditeShi N, Ma Z, Liu W (1991) Crystal structure determination of ankangite with one dimensional incommensurate modulation Acta Petrologica et Mineralogica 10 233-2451991Shiti barite deposit, Ankang County, Shaanxi, China0293
0018318MannarditeShi N, Ma Z, Liu W (1991) Crystal structure determination of ankangite with one dimensional incommensurate modulation Acta Petrologica et Mineralogica 10 233-2451991Shiti barite deposit, Ankang County, Shaanxi, China0293
0009328MannarditeShi-bin X, Hai-fu F, Xiao-jing W, Fang-hua L (1990) Direct methods in superspace. II The first application to an unknown incommensurate modulated structure Acta Crystallographica A46 929-9341990Shiti barite deposit, Ankang County, Shaanxi, China0293
0005210MannarditeSzymanski J T (1986) The crystal structure of mannardite, a new hydrated cryptomelane-group (hollandite) mineral with a doubled short axis The Canadian Mineralogist 24 67-7819860293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.201 Å(100) 420
1.586 Å(80) 732
2.473 Å(70) 312
1.887 Å(70) 352
2.224 Å(50) 332

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 3a: Earth’s earliest Hadean crust>4.50
7 : Ultramafic igneous rocks
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Type Occurrence of MannarditeHide

General Appearance of Type Material:
Millimetre-sized euhedral black crystals.
Place of Conservation of Type Material:
Geological Survey of Canada, Ottawa, Ontario, Canada, 64197.
Royal Ontario Museum, Toronto, Canada, M40292, M40293.
The Natural History Museum, London, England, 1983,68 and 1983,69.
National Museum of Natural History, Washington, D.C., USA, 150275, 150337, 162567.
Geological Setting of Type Material:
Geological setting is represented by quartz veins embedded in the Gunsteel Fm., a paleozoic formation rich in baryte. Mannardite was found in three different kind of veins: type A, in association with barytocalcite and norsethite; type B, in which almost barytocalcite has been altered to baryte, in association with rare norsethite and sulvanite; type C, only with quartz and barytocalcite.
Associated Minerals at Type Locality:

Synonyms of MannarditeHide

Other Language Names for MannarditeHide

German:Mannardit
Simplified Chinese:曼纳德石
Spanish:Mannardita

Relationship of Mannardite to other SpeciesHide

Other Members of Priderite Group:
HenrymeyeriteBa(Ti4+7Fe2+)O16Tet. 4/m : I4/m
KopernikiteK(Ti7Cr3+)O16Tet. 4/m : I4/m
PrideriteK(Ti4+7Fe3+)O16Tet. 4/m : I4/m
RedledgeiteBa(Ti4+6Cr3+2)O16Tet.
'UM1994-09-O:CrKTi'Compare UM1994-07-O:BaCrFeMgTi and UM1994-08-O:CaFeKMgTi.

Common AssociatesHide

Associations Based on Photo Data:
9 photos of Mannardite associated with QuartzSiO2
4 photos of Mannardite associated with ZinkenitePb9Sb22S42
2 photos of Mannardite associated with BaryteBaSO4
1 photo of Mannardite associated with PectoliteNaCa2Si3O8(OH)

Related Minerals - Strunz-mindat GroupingHide

4.DK.KThalliomelaneTl(Mn4+7.5Cu2+0.5)O16Tet. 4/m : I4/m
4.DK.FerrihollanditeBa(Mn4+6Fe3+2)O16Mon. 2/m
4.DK.KopernikiteK(Ti7Cr3+)O16Tet. 4/m : I4/m
4.DK.4.DK.FerricoronaditePb(Mn4+6Fe3+2)O16Tet. 4/m : I4/m
4.DK.05aManjiroiteNa(Mn4+7Mn3+)O16Tet. 4/m : I4/m
4.DK.05bRedledgeiteBa(Ti4+6Cr3+2)O16Tet.
4.DK.05Akaganeite(Fe3+,Ni2+)8(OH,O)16Cl1.25 · nH2OMon. 2/m
4.DK.05aCoronaditePb(Mn4+6Mn3+2)O16Mon. 2/m
4.DK.05aHollanditeBa(Mn4+6Mn3+2)O16Mon. 2/m
4.DK.05aCryptomelaneK(Mn4+7Mn3+)O16Mon. 2/m
4.DK.05aStrontiomelaneSr(Mn4+6Mn3+2)O16Mon. 2/m : P21/b
4.DK.05bHenrymeyeriteBa(Ti4+7Fe2+)O16Tet. 4/m : I4/m
4.DK.05bPrideriteK(Ti4+7Fe3+)O16Tet. 4/m : I4/m
4.DK.10Romanèchite(Ba,H2O)2(Mn4+,Mn3+)5O10Mon. 2/m
4.DK.10Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2OMon. 2/m : P2/m

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for MannarditeHide

References for MannarditeHide

Reference List:

Localities for MannarditeHide

Showing 25 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Brazil
 
  • Minas Gerais
Dr Jaroslav Hyrsl specimen
Tony Nikischer specimen and analysis +1 other reference
Canada (TL)
 
  • British Columbia
    • Liard Mining Division
      • Sifton Pass
        • Kechika River
Scott et al. (1986) +1 other reference
  • New Brunswick
    • Gloucester Co.
      • Bathurst Parish
        • Bathurst Mining Camp
Scott et al. (1986)
China
 
  • Jiangxi
    • Jiujiang
Yang et al. (2024)
Yang et al. (2024)
Yang et al. (2024)
Yang et al. (2024)
Yang et al. (2026)
  • Shaanxi
    • Ankang
      • Hanbin District
Xiong Ming et al. (1988) +1 other reference
  • Sichuan
    • Garzê Autonomous Prefecture (Ganzi Autonomous Prefecture)
      • Baiyü County
        • Maqiong
Fengyi Chen et al. (1984) +2 other references
Italy
 
  • Tuscany
    • Lucca Province
      • Stazzema
        • Sant'Anna di Stazzema
Biagioni et al. (2008) +1 other reference
Japan
 
  • Gunma Prefecture
    • Kiryu City
Nagashima et al. (2026)
Kazakhstan
 
  • Kyzylorda Region
    • Shieli District
Karpenko et al. (2011)
  • Turkistan Region
    • Sozak District
      • Aksumbe
Karpenko et al. (2011)
      • Budenovskoye Uranium ore field
Uranium One
Kyrgyzstan
 
  • Batken Region
    • Kadamjay District
Karpenko et al. (2011)
Karpenko et al. (2011)
Poland
 
  • Lower Silesian Voivodeship
    • Wrocław County
      • Gmina Kobierzyce
Ł. Kruszewski PXRD & pXRF data (paper in preparation)
Russia
 
  • Irkutsk Oblast
    • Slyudyansky District
      • Slyudyanka
Proceedings of the Russian Mineralogical Society 136 (5) +3 other references
  • Khakassia (Republic of Khakassia)
    • Askizsky Rayon
      • Askiz ore district
Kassandrov et al. (2009)
Kassandrov et al. (2009)
  • Murmansk Oblast
Menshikov et al. (2015)
South Africa
 
  • Free State
    • Lejweleputswa District Municipality
      • Masilonyana Local Municipality
        • Theunissen
          • Theunissen kimberlite field
Mitchell et al. (1989) +1 other reference
 
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