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Pyrrhotite

A valid IMA mineral species - grandfathered
This page kindly sponsored byMark Kucera
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Named in 1847 by Ours-Pierre-Armand Petit-Dufrénoy from Greek πνρρός "pyrrhos", flame-colored.
Pyrrhotite is found withpentlandite in basic igneous rocks, veins, and metamorphic rocks. It is also often found with pyrite, marcasite, and magnetite. It has varying magnetic powers, depending on the number of Fe vacancies in the crystal structure. A related species with no vacancies (and therefore non-magnetic), is calledtroilite and has been found in meteorites and rarely terrestrially.

Several polytypes are known; the most common one ispyrrhotite-4C.

Visually similar tosmythite andtroilite.

Compare'UM1989-25-S:FeNi' - a representative of the Fe1-xS-Ni1-xS (Mss) solid solution.


Unique Identifiers
IMA Formula:
Fe7S8

Classification of Pyrrhotite

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
C : Metal Sulfides, M: S = 1: 1 (and similar)
C : With Ni, Fe, Co, PGE, etc.
2.8.10.1

2 : SULFIDES
8 : AmXp, with m:p = 1:1
3.9.1

3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
9 : Sulphides etc. of Fe

Mineral SymbolsJolyon RalphUnited Kingdom

Physical Properties of Pyrrhotite
Transparency:
Opaque
Colour:
Bronze brown, bronze red, or dark brown
Comment:
Tarnishes quickly
Streak:
Dark grayish black
Hardness:
VHN100=373 - 409 kg/mm2 - Vickers
Cleavage:
None Observed
Parting:
Distinct on {0001}
Fracture:
Sub-Conchoidal
Density:
4.58 - 4.65 g/cm3 (Measured)    4.69 g/cm3 (Calculated)

Optical Data of Pyrrhotite
Common Impurities:
Ni,Co,Cu

Chemical Analysis
Click on an icon to view
Pyrrhotite no.15 - Goldschmidt (1913-1926)
Pyrrhotite - Contact twin on {10-12}
Pyrrhotite - {100}, {001}
Pyrrhotite - {101}, {001}
3d models and HTML5 code kindly provided bywww.smorf.nl.

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Edge Lines |Miller Indices |Axes

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Opaque |Translucent |Transparent

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Crystal Structure
Epitaxy Comments:
Usually, the pyrrhotite is on the galena, but codepositing intergrowths are known. The "six-fold" axis of pyrrhotite is parallel to the three-fold axis (octahedral axis) in galena.

X-Ray Powder Diffraction

Other Language Names for Pyrrhotite

Varieties of PyrrhotiteNickel-bearing PyrrhotiteA nickel-bearing variety of pyrrhotite.
Note, however, that there are several iron-nickel sulphides.

Relationship of Pyrrhotite to other Species
Other Members of Pyrrhotite Group:
Smythite(Fe,Ni)3+xS4 (x=0-0.3)Trig.3m(32/m) :R3m
TroiliteFeSHex. 6/mmm(6/m2/m2/m) :P63/mmc

Common AssociatesTrig. 32 :P32212.CC.TilkerodeitePd2HgSe3Trig.3m(32/m) :P3m12.CC.UM2007-26-S:CuFeIrNiPtRh(Ir,Cu,Ni,Pt,Rh,Fe)9S112.CC.Proxitwelvefoldite Pd3Ni4Te8Tet. 4/mmm(4/m2/m2/m) :P42/mnm2.CC.FerrotorryweiseriteRh5Fe10S16Trig.3m(32/m) :R3m2.CC.TamuraiteIr5Fe10S16Trig.3m(32/m) :R3m2.CC.Crowningshieldite(Ni0.9Fe0.1)SHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.KuvaeviteIr5Ni10S16Trig.3m(32/m) :R3m2.CC.TorryweiseriteRh5Ni10S16Trig.3m(32/m) :R3m2.CC.05AchávaliteFeSeHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.05LangisiteCoAsHex. 6 :P632.CC.05SederholmiteNiSeHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.05FrebolditeCoSeHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.05NickelineNiAsHex. 6/mmm(6/m2/m2/m) :P63/mcm2.CC.05SobolevskitePdBiHex.2.CC.05JaipuriteCoSHex.2.CC.05KotulskitePd(Te,Bi)2-x (x ≈ 0.4)Hex.2.CC.05ZlatogoriteNiCuSb2Trig.3m(32/m) :P31m2.CC.05StumpflitePtSbHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.05SudburyitePdSbHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.05BreithauptiteNiSbHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.10Smythite(Fe,Ni)3+xS4 (x=0-0.3)Trig.3m(32/m) :R3m2.CC.10TroiliteFeSHex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.15Ruthenarsenite(Ru,Ni)AsOrth.mmm(2/m2/m2/m) :Pnma2.CC.15Westerveldite(Fe,Ni,Co)AsOrth.mmm(2/m2/m2/m)2.CC.15ModderiteCoAsOrth.mmm(2/m2/m2/m)2.CC.15MinakawaiteRhSbOrth.mmm(2/m2/m2/m) :Pnma2.CC.15CherepanoviteRhAsOrth.mmm(2/m2/m2/m) :Pnma2.CC.20UM1990-38-S:CuFeIrNiPtRh(Ni,Fe,Rh,Cu,Ir,Pt)S2.CC.20MilleriteNiSTrig. 3m :R3m2.CC.20MäkineniteNiSeTrig. 3m2.CC.25MackinawiteFeSTet. 4/mmm(4/m2/m2/m) :P4/nmm2.CC.30VavříniteNi2SbTe2Hex. 6/mmm(6/m2/m2/m) :P63/mmc2.CC.30Hexatestibiopanickelite(Pd,Ni)(Sb,Te) ?Hex.2.CC.35bCooperitePtSTet. 4/mmm(4/m2/m2/m) :P42/mmc2.CC.35aVysotskitePdSTet. 4/m :P42/m2.CC.35aBraggitePdPt3S4Tet. 4/m :P42/m2.CC.45JacutingaitePt2HgSe3Trig.3m(32/m) :P3m12.CC.50ImgreiteNiTe (?)Hex.

Fluorescence of Pyrrhotite

Other InformationCoarse-grained-ultramafic-rock

Internet Links for Pyrrhotite
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  • Look for Pyrrhotite in the Rock H. Currier Digital Library
  • References for PyrrhotiteRamsden, A.R. (1975) Compositions of coexisting pyrrhotites, pentlandites and pyrites at Spargoville, Western Australia. The Canadian Mineralogist: 13: 133-137.

    Significant localities for PyrrhotiteRenison Bell MineKitto+4 other references
    Brazil
     
    Rocks & Min.: 63:43+2 other references
    Canada
     
    Grice et al. (1977)+1 other referenceTavchandjian (1992)
    Italy
     
    Benvenuti et al. (2000)
    Japan
     
    - (1911)+2 other references
    Kosovo
     
    Féraud J. (1979)+4 other references
    Mexico
     
    Panczner (1987)
    Norway
     
    Neumann (1944)Vogt (1900)+1 other reference
    Peru
     
    Imai et al. (1985)+1 other reference
    Romania
     
    Palache et al. (1944)+4 other references
    Russia
     
    Dobovol'skaya et al. (1990)+3 other references
    Switzerland
     
    Ansermet (2004)+3 other references
    USA
     
    Ague (1995)+1 other reference
     
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