Trigonite (original) (raw)

A valid IMA mineral species - grandfathered

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About TrigoniteHide

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Formula:

Pb3Mn2+(AsO3)2(HAsO3)

Colour:

Yellow to yellow-brown, dark brown or black; pale yellow to brownish yellow in transmitted light

Lustre:

Adamantine, Vitreous

Specific Gravity:

6.1 - 7.1

Crystal System:

Monoclinic

Name:

From the Greek τρίγωνον, "trigonon", a triangle, alluding to its common crystal shape.

This page provides mineralogical data about Trigonite.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:4016:3

7dc9ccaa-324f-4705-bec1-fb36f09b63c7

IMA Classification of TrigoniteHide

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Approved, 'Grandfathered' (first described prior to 1959)

IMA Formula:

Pb3Mn2+(AsO3)2(AsO2OH)

Classification of TrigoniteHide

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4.JB.40

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
B : Arsenites, antimonites, bismuthites; with additional anions, without H2O

45.1.2.1

45 : ACID AND NORMAL ANTIMONITES AND ARSENITES
1 : Miscellaneous

Mineral SymbolsHide

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

Symbol Source Reference
Tgn IMA–CNMNC Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of TrigoniteHide

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Colour:

Yellow to yellow-brown, dark brown or black; pale yellow to brownish yellow in transmitted light

Cleavage:

Perfect
On {010}, perfect; on {101}, good.

Fracture:

Irregular/Uneven

Density:

6.1 - 7.1 g/cm3 (Measured) 6.35 g/cm3 (Calculated)

Optical Data of TrigoniteHide

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RI values:

_n_α = 2.070 _n_β = 2.100 _n_γ = 2.120

δ = 0.050

Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.

Optical Extinction:

Y = b.

Chemistry of TrigoniteHide

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Mindat Formula:

Pb3Mn2+(AsO3)2(HAsO3)

Crystallography of TrigoniteHide

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Crystal System:

Monoclinic

Cell Parameters:

a = 7.258 Å, b = 6.822 Å, c = 11.088 Å
β = 91.45°

Ratio:

a:b:c = 1.064 : 1 : 1.625

Unit Cell V:

548.84 ų (Calculated from Unit Cell)

Morphology:

Crystals domatic with a trigonal outline from the development of numerous domatic forms including c _s, and _p; also complexly modified; thick tabular, flattened on {010}; subparallel growths.

Crystal StructureHide

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ID Species Reference Link Year Locality Pressure (GPa) Temp (K)
0015671 Trigonite Pertlik F (1978) The crystal structure of trigonite, Pb3Mn(AsO3)2(AsO2(OH)) Tschermaks Mineralogische und Petrographische Mitteilungen 25 95-105 1978 Langban, Varmland, Sweden 0 293

CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
2.99 Å (100)
3.08 Å (90)
3.24 Å (70)
4.90 Å (60)
4.50 Å (40)
3.65 Å (40)
2.76 Å (40)

Comments:

Långban Mine, Sweden.

Geological EnvironmentHide

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Type Occurrence of TrigoniteHide

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Place of Conservation of Type Material:

Swedish Museum of Natural History, Stockholm, Sweden.

Geological Setting of Type Material:

Metamorphosed Fe-Mn ore body.

Associated Minerals at Type Locality:

Other Language Names for TrigoniteHide

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Common AssociatesHide

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Associated Minerals Based on Photo Data:

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4.JB. Cuyaite Ca2Mn3+As3+14O24Cl Mon. m
4.JB. Brattforsite Mn19(AsO 3)12Cl2 Mon. 2/m : _B_2/b
4.JB.05 Fetiasite (Fe3+,Fe2+,Ti)3(As2O5)O2 Mon. 2/m : _P_21/m
4.JB.10 Manganarsite Mn3(As2O4)(OH)4 Trig.
4.JB.15 UM1984-09-AsO:ClHMn Mn10As6O18(OH)Cl Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a c d
4.JB.15 Magnussonite Mn2+10(As3+O3)6(OH,Cl)2 Iso. m_3_m _(_4/_m_32/m ) : I a_3_d
4.JB.20 Armangite Mn2+26(AsO3)14(HAsO3)4(CO3) Trig. 3 : _P_3
4.JB.25 Nanlingite Na(Ca5Li)Mg12(AsO3)2[Fe(AsO3)6]F14 Trig. 3_m_ _(_32/m ) : R_3_m
4.JB.30 Asbecasite Ca3(Ti,Sn4+)Be2(AsO3)6(SiO4)2 Trig. 3_m_ : _P_3_c_1
4.JB.35 Stenhuggarite CaFeSb(AsO3)2O Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d
4.JB.45 Finnemanite Pb5(AsO3)3Cl Hex. 6/m : _P_63/m
4.JB.50 Gebhardite Pb8(As2O5)2OCl6 Mon. 2/m : _P_21/b
4.JB.55 Graeserite Fe3+4Ti3As3+O13(OH) Mon. 2/m : _B_2/m
4.JB.55 Tomichite (V,Fe)4Ti3AsO13(OH) Mon. 2/m : _P_21/m
4.JB.55 Derbylite Fe3+4Ti3Sb3+O13(OH) Mon. 2/m : _P_21/m
4.JB.60 Hemloite (Ti,V3+,Fe3+,Al)12(As3+,Sb3+)2O23(OH) Tric. 1 : _P_1
4.JB.65 Freedite Cu+Pb8(AsO3)2O3Cl5 Mon. 2/m : _B_2/m
4.JB.70 Georgiadesite Pb4(As3+O3)Cl4(OH) Mon. 2/m : _P_21/b
4.JB.75 Szklaryite ◻Al6BAs3+3O15 Orth. m m m _(_2/_m_2/_m_2/m ) : P b c m
4.JB.75 Ekatite (Fe3+,Fe2+,Zn)12(AsO3)6(AsO3,HSiO4)2(OH)6 Hex. 6_m_ m : P_63_m c
4.JB.85 Lepageite Mn2+3(Fe3+7Fe2+4)O3[Sb3+5As3+8O34] Tric. 1 : _P_1
4.JB.90 Bianchiniite Ba2(TiV)(As2O5)2OF Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_4/m c m

Other InformationHide

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Notes:

Soluble in dilute acids.

Health Risks:

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

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References for TrigoniteHide

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Localities for TrigoniteHide

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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.

Locality ListHide

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- 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.

Sweden (TL)
Värmland County Filipstad Långban Ore District Långban Mine (TL) Geologiska Föreningens I Stockholm. Förhandlinger (1920) +3 other references