Pyrrhotite (original) (raw)
A valid IMA mineral species - grandfathered
About PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Also given as Fe1-x (x = 0 to 0.17). The various polytypes known have slightly different stoichiometries.
Colour:
Bronze brown, bronze red, or dark brown
Specific Gravity:
4.58 - 4.65
Crystal System:
Monoclinic
Name:
Named in 1847 by Ours-Pierre-Armand Petit-Dufrénoy from Greek πνρρός "pyrrhos", flame-colored.
Pyrrhotite is found with pentlandite 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 called troilite and has been found in meteorites and rarely terrestrially.
Several polytypes are known; the most common one is pyrrhotite-4C.
Visually similar to smythite and troilite.
Compare 'UM1989-25-S:FeNi' - a representative of the Fe1-xS-Ni1-xS (Mss) solid solution.
Unique IdentifiersHide
This section is currently hidden. Click the show button to view.
Long-form identifier:
mindat:1:1:3328:8
2b5c1e78-dfac-47e8-b3f8-ed5489951809
IMA Classification of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Approved, 'Grandfathered' (first described prior to 1959)
Classification of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
2.CC.10
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 SymbolsHide
This section is currently hidden. Click the show button to view.
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Pyh | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Po | Kretz (1983) | Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279. |
Po | Siivolam & Schmid (2007) | Siivolam, J. and Schmid, R. (2007) Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: List of mineral abbreviations. Web-version 01.02.07. IUGS Commission on the Systematics in Petrology. download |
Po | Whitney & Evans (2010) | Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371 |
Po | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Pyh | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Pronunciation of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Pronunciation:
Play | Recorded by | Country |
---|---|---|
Sorry, your browser doesn't support HTML5 audio. | Jolyon Ralph | United Kingdom |
Physical Properties of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Colour:
Bronze brown, bronze red, or dark brown
Comment:
Tarnishes quickly
Streak:
Dark grayish black
Hardness:
VHN100=373 - 409 kg/mm2 - Vickers
Parting:
Distinct on {0001}
Density:
4.58 - 4.65 g/cm3 (Measured) 4.69 g/cm3 (Calculated)
Optical Data of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 27.9% | 31.0% |
420nm | 28.6% | 32.2% |
440nm | 29.4% | 33.6% |
460nm | 30.3% | 34.8% |
480nm | 31.4% | 36.2% |
500nm | 32.4% | 37.6% |
520nm | 33.4% | 38.6% |
540nm | 34.5% | 39.6% |
560nm | 35.5% | 40.4% |
580nm | 36.5% | 41.2% |
600nm | 37.4% | 42.0% |
620nm | 38.3% | 42.6% |
640nm | 39.1% | 43.0% |
660nm | 39.9% | 43.5% |
680nm | 40.7% | 43.9% |
700nm | 41.4% | 44.1% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 44.1%.
R1 shown in black, R2 shown in red
Chemistry of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Mindat Formula:
Fe1-xS
Also given as Fe1-x (x = 0 to 0.17). The various polytypes known have slightly different stoichiometries.
Common Impurities:
Ni,Co,Cu
Crystallography of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Pyrrhotite-11C | Pyrrhotite-4C | Pyrrhotite-5C | Pyrrhotite-6C | Pyrrhotite-7H |
---|---|---|---|---|
Fe10S11 | Fe7S8 | Fe9S10 | Fe11S12 | Fe9S10 |
Orthorhombic | Monoclinic | Monoclinic | Monoclinic | Hexagonal |
2/m - Prismatic | 2 - Sphenoidal | m - Domatic | ||
_B_2/b | _P_21 | B b | ||
_C_2/c | _P_21 | C c | ||
a = 3.433(9) Å, b = 5.99(2) Å, c = 5.7432(5) Åβ = 90° | a = 11.88 Å, b = 6.87 Å, c = 22.79 Åβ = 90.47° | a = 6.8673(4) Å, b = 28.6536(9) Å, c = 6.8592(4) Åβ = 119.975(7)° | a = 6.8973(15) Å, b = 11.954(3) Å, c = 17.602(4) Åα = 90°, β = 101.302(4)°, γ = 90° | |
a:b:c = 0.573 : 1 : 0.959 | a:b:c = 1.729 : 1 : 3.317 | a:b:c = 0.24 : 1 : 0.239 | a:b:c = 0.577 : 1 : 1.472 | |
V 118.10 ų(Calculated from Unit Cell) | V 1,859.96 ų(Calculated from Unit Cell) | V 1169.18 ų | V 1423.1 ų | |
4 | 4 |
Crystallographic forms of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Crystal Atlas:
Image Loading
3d models and HTML5 code kindly provided bywww.smorf.nl.
Toggle
Edge Lines |Miller Indices |Axes
Transparency
Opaque |Translucent |Transparent
View
Along a-axis |Along b-axis |Along c-axis |Start rotation |Stop rotation
Crystal StructureHide
This section is currently hidden. Click the show button to view.
Load
Unit Cell |Unit Cell Packed
2x2x2 |3x3x3 |4x4x4
Show
Big Balls |Small Balls |Just Balls |Spacefill
Polyhedra Off |Si Polyhedra |All Polyhedra
Remove metal-metal sticks
Display Options
Black Background |White Background
Perspective On |Perspective Off
2D |Stereo |Red-Blue |Red-Cyan
View
CIF File Best |x |y |z |a |b |c
Rotation
Stop |Start
Labels
Console Off |On |Grey |Yellow
ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0000288 | Pyrrhotite | Tokonami M, Nishiguchi K, Morimoto N (1972) Crystal structure of a monoclinic pyrrhotite (Fe7S8) American Mineralogist 57 1066-1080 | 1972 | 0 | 293 | ||
0020728 | Pyrrhotite | Liles D C, de Villiers J P R (2012) Redetermination of structure of 5C pyrrhotite at low temperature and at room temperature American Mineralogist 97 257-261 | 2012 | Silberberg mine, Bodenmais, Germany | 0 | 120 | |
0020729 | Pyrrhotite | Liles D C, de Villiers J P R (2012) Redetermination of structure of 5C pyrrhotite at low temperature and at room temperature American Mineralogist 97 257-261 | 2012 | Silberberg mine, Bodenmais, Germany | 0 | 293 | |
0020730 | Pyrrhotite | Liles D C, de Villiers J P R (2012) Redetermination of structure of 5C pyrrhotite at low temperature and at room temperature American Mineralogist 97 257-261 | 2012 | Copper Cliff mine, Sudbury, Canada | 0 | 293 | |
0004985 | Pyrrhotite | de Villiers J P R, Liles D C, Becker M (2009) The crystal structure of a naturally occurring 5C pyrrhotite from Sudbury, its chemistry, and vacancy distribution American Mineralogist 94 1405-1410 | 2009 | Copper Cliff North Mine, Sudbury, Canada | 0 | 293 | |
0005000 | Pyrrhotite | De Villiers J P R, Liles D C (2010) The crystal-structure and vacancy distribution in 6C pyrrhotite American Mineralogist 95 148-152 | 2010 | Mponeng Mine, South Africa | 0 | 293 | |
0005001 | Pyrrhotite | De Villiers J P R, Liles D C (2010) The crystal-structure and vacancy distribution in 6C pyrrhotite American Mineralogist 95 148-152 | 2010 | Mponeng Mine, South Africa | 0 | 293 | |
0018053 | Pyrrhotite | Alsen N (1925) Roentgenographische Untersuchungen der Kristallstrukturen von Magnetkies, Breithauptit, Pentlandit, Millerit und verwandten Verbindungen _cod_database_code 1011178 Geologiska Foreningens i Stockholm Forhandlingar 47 19-73 | 1925 | 0 | 293 | ||
0018054 | Pyrrhotite | Alsen N (1925) Roentgenographische Untersuchungen der Kristallstrukturen von Magnetkies, Breithauptit, Pentlandit, Millerit und verwandten Verbindungen _cod_database_code 1011179 Geologiska Foreningens i Stockholm Forhandlingar 47 19-73 | 1925 | 0 | 293 | ||
0020604 | Pyrrhotite | Powell A V, Vaqueiro P, Knight K S, Chapon L C, Sanchez R D (2004) Structure and magnetism in synthetic pyrrhotite Fe7S8: A powder neutron-diffraction study Physical Review B70 014415-12 | 2004 | Synthetic | 0 | 11 | |
0020605 | Pyrrhotite | Powell A V, Vaqueiro P, Knight K S, Chapon L C, Sanchez R D (2004) Structure and magnetism in synthetic pyrrhotite Fe7S8: A powder neutron-diffraction study Physical Review B70 014415-12 | 2004 | Synthetic | 0 | 298 |
CIF Raw Data - click here to close
Epitaxial Relationships of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
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 DiffractionHide
This section is currently hidden. Click the show button to view.
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
5.94 Å | (10) |
5.72 Å | (20) |
5.27 Å | (7) |
3.44 Å | (7) |
2.98 Å | (40) |
2.87 Å | (10) |
2.64 Å | (50) |
2.255 Å | (10) |
2.207 Å | (7) |
2.064 Å | (100) |
1.987 Å | (7) |
1.909 Å | (7) |
1.769 Å | (7) |
1.720 Å | (40) |
1.636 Å | (10) |
1.606 Å | (7) |
1.490 Å | (10) |
1.476 Å | (7) |
1.442 Å | (10) |
1.433 Å | (20) |
1.321 Å | (20) |
1.291 Å | (10) |
1.174 Å | (10) |
1.167 Å | (7) |
1.125 Å | (7) |
1.105 Å | (15) |
1.101 Å | (10) |
1.065 Å | (7) |
1.048 Å | (10) |
0.993 Å | (7) |
0.979 Å | (7) |
Comments:
ICDD 22-1120 (4C polytype). See also ICDD 29-723 (4C polytype), and 24-79/24-79a (4C polytype). Data for other polytypes include: ICDD 25-411 (1C polytype); ICDD 24-220 (3C polytype); ICDD 29-724 (5C polytype); ICDD 29-725 (6C polytype); ICDD 20-534 (7C polytype); and ICDD 29-726 (11C polytype).
Geological EnvironmentHide
This section is currently hidden. Click the show button to view.
Synonyms of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Other Language Names for PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Simplified Chinese:磁黄铁矿
Traditional Chinese:磁黃鐵礦
Varieties of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Relationship of Pyrrhotite to other SpeciesHide
This section is currently hidden. Click the show button to view.
Other Members of this group:
Smythite | (Fe,Ni)3+xS4 (x=0-0.3) | Trig. 3_m_ _(_32/m ) : R_3_m |
---|---|---|
Troilite | FeS | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
Common AssociatesHide
This section is currently hidden. Click the show button to view.
Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
This section is currently hidden. Click the show button to view.
2.CC. | Tilkerodeite | Pd2HgSe3 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
---|---|---|---|
2.CC. | UM2007-26-S:CuFeIrNiPtRh | (Ir,Cu,Ni,Pt,Rh,Fe)9S11 | |
2.CC. | Crowningshieldite | (Ni0.9Fe0.1)S | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC. | Eliopoulosite | V7S8 | Trig. 32 : _P_3221 |
2.CC. | Kuvaevite | Ir5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Torryweiserite | Rh5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Tamuraite | Ir5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Ferrotorryweiserite | Rh5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Proxitwelvefoldite | Pd3Ni4Te8 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_42/m n m |
2.CC.05 | Achávalite | FeSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Breithauptite | NiSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Freboldite | CoSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Kotulskite | Pd(Te,Bi)2-x (x ≈ 0.4) | Hex. |
2.CC.05 | Langisite | CoAs | Hex. 6 : _P_63 |
2.CC.05 | Nickeline | NiAs | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m c m |
2.CC.05 | Sederholmite | beta-NiSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sobolevskite | PdBi | Hex. |
2.CC.05 | Stumpflite | PtSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sudburyite | PdSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Jaipurite | CoS | Hex. |
2.CC.05 | Zlatogorite | NiCuSb2 | Trig. 3_m_ _(_32/m ) : P_31_m |
2.CC.10 | Smythite | (Fe,Ni)3+xS4 (x=0-0.3) | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC.10 | Troilite | FeS | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.15 | Cherepanovite | RhAs | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.15 | Modderite | (Co,Fe)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Ruthenarsenite | (Ru,Ni)As | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.15 | Westerveldite | (Fe,Ni,Co)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Minakawaite | RhSb | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.20 | Millerite | NiS | Trig. 3_m_ : R_3_m |
2.CC.20 | Mäkinenite | γ-NiSe | Trig. 3_m_ |
2.CC.20 | UM1990-38-S:CuFeIrNiPtRh | (Ni,Fe,Rh,Cu,Ir,Pt)S | |
2.CC.25 | Mackinawite | FeS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n m m |
2.CC.30 | Hexatestibiopanickelite | (Pd,Ni)(Sb,Te) ? | Hex. |
2.CC.30 | Vavřínite | Ni2SbTe2 | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.35a | Braggite | PdPt3S4 | Tet. 4/m : _P_42/m |
2.CC.35b | Cooperite | PtS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_42/m m c |
2.CC.35a | Vysotskite | PdS | Tet. 4/m : _P_42/m |
2.CC.45 | Jacutingaite | Pt2HgSe3 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
2.CC.50 | Imgreite | NiTe (?) | Hex. |
Fluorescence of PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Other InformationHide
This section is currently hidden. Click the show button to view.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Pyrrhotite in petrologyHide
This section is currently hidden. Click the show button to view.
An essential component of rock names highlighted in red, an accessory component in rock names highlighted in green.
Internet Links for PyrrhotiteHide
This section is currently hidden. Click the show button to view.
References for PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Reference List:
Barkov, A. Y., Laajoki, K. V. O., Men'shikov, Y. P., Alapieti, T. T., Sivonen, S. J. (1997) First terrestrial occurrence of titanium-rich pyrrhotite, marcasite and pyrite in a fenitized xenolith from the Khibina alkaline complex, Russia. The Canadian Mineralogist, 35 (4) 875-885
Tan, Zheng, Su, Xuping, Li, Zhi, Liu, Ya, Wang, Jianhua (2007) Phase equilibria in the Zn–Fe–S system at 450°C. International Journal of Materials Research, 98 (1) 16-20 doi:10.3139/146.101435
Significant localities for PyrrhotiteHide
This section is currently hidden. Click the show button to view.
Showing 13 significant localities out of 11,215 recorded on mindat.org.
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
This section is currently hidden. Click the show button to view.
- 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.