Arsenopyrite (original) (raw)
A valid IMA mineral species - grandfathered
About ArsenopyriteHide
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Colour:
Silver-white to steel-gray, may have a slight yellow appearance
Lustre:
Metallic, Sub-Metallic
Crystal System:
Monoclinic
Name:
Named in 1847 by Ernst Friedrich Glocker for its composition, a contraction of the antiquated term "arsenical pyrite." Arsenopyrite was known much before 1847 and arsenopyrite, as a name, may be taken as a simple translation of "arsenkies".
Arsenopyrite is closely related to alloclasite, but is not an exact analogue, because of different As-S and S-As ordering.
Arsenopyrite may contain up to about 9 wt% Co; with higher Co contents, glaucodot will appear as a separate phase (Gammon, 1966).
May be confused with the iron arsenide löllingite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:305:8
IMA Classification of ArsenopyriteHide
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Approved, 'Grandfathered' (first described prior to 1959)
Classification of ArsenopyriteHide
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2.EB.20
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
E : Metal Sulfides, M: S <= 1:2
B : M:S = 1:2, with Fe, Co, Ni, PGE, etc.
2.12.4.1
2 : SULFIDES
12 : AmBnXp, with (m+n):p = 1:2
3.9.12
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
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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.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Apy | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Apy | Kretz (1983) | Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279. |
Apy | 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 |
Apy | 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 |
Apy | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of ArsenopyriteHide
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Colour:
Silver-white to steel-gray, may have a slight yellow appearance
Comment:
Tarnished material common
Hardness:
VHN100=1081 kg/mm2 - Vickers
Comment:
VHN on (001) section
Cleavage:
Distinct/Good
Distinct on {001}; {010} in traces
Fracture:
Irregular/Uneven
Density:
6.07(15) g/cm3 (Measured) 6.18 g/cm3 (Calculated)
Optical Data of ArsenopyriteHide
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Anisotropism:
Strong red-violet
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 50.3% | 51.8% |
420nm | 50.3% | 51.8% |
440nm | 51.3% | 51.8% |
460nm | 50.6% | 51.8% |
480nm | 51.0% | 51.9% |
500nm | 51.4% | 51.9% |
520nm | 51.8% | 51.9% |
540nm | 52.2% | 51.9% |
560nm | 52.5% | 51.9% |
580nm | 53.0% | 51.8% |
600nm | 53.4% | 51.6% |
620nm | 53.6% | 51.5% |
640nm | 53.6% | 51.3% |
660nm | 53.6% | 51.3% |
680nm | 53.4% | 51.2% |
700nm | 53.2% | 51.0% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 53.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
White with faint yellow tint
Comments:
White or bluish tint, faint reddish yellow
Chemistry of ArsenopyriteHide
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Common Impurities:
Ag,Au,Co,Sn,Ni,Sb,Bi,Cu,Pb
Crystallography of ArsenopyriteHide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 5.7612(8) Å, b = 5.6841(7) Å, c = 5.7674(8) Å
β = 111.721(8)°
Ratio:
a:b:c = 1.014 : 1 : 1.015
Morphology:
Flat tabular to blocky (sometimes pseudo-octahedral) to prismatic.
Twinning:
Common on {100} and {001}. Contact or penetration on {101}, on {012} trillings or cruciform.
Comment:
Cell parameters from Bindi et al. (2012), using stoichiometric crystals. Pseudo-orthorhombic, face-centred cell: ~5.7, ~6.4, ~9.6 A.
Crystallographic forms of ArsenopyriteHide
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Crystal Atlas:
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Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0000112 | Arsenopyrite | Morimoto N, Clark L A (1961) Arsenopyrite crystal-chemical relations From Freiberg, Germany American Mineralogist 46 1448-1469 | ![]() |
1961 | 0 | 293 | |
0019195 | Arsenopyrite | Bindi L, Moelo Y, Leone P, Suchaud M (2012) Stoichiometric arsenopyrite, FeAsS, from La Roche-Balue Quarry, Loire-Atlantique, France: Crystal structure and Mossbauer study The Canadian Mineralogist 50 471-479 | 2012 | La Roche-Balue Quarry, Loire-Atlantique, France | 0 | 293 | |
0016964 | Arsenopyrite | Buerger M (1936) The symmetry and crystal structure of the minerals of the arsenopyrite group Zeitschrift fur Kristallographie 95 83-113 | ![]() |
1936 | St Peter mine, Spindelmuhle, Bohemia | 0 | 293 |
0010966 | Arsenopyrite | Fuess H, Kratz T, Topel-Schadt J, Miehe G (1987) Crystal structure refinement and electron microscopy of arsenopyrite Zeitschrift fur Kristallographie 179 335-346 | ![]() |
1987 | Hakansboda, Sweden | 0 | 293 |
0010967 | Arsenopyrite | Fuess H, Kratz T, Topel-Schadt J, Miehe G (1987) Crystal structure refinement and electron microscopy of arsenopyrite Zeitschrift fur Kristallographie 179 335-346 | ![]() |
1987 | Hakansboda, Sweden | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Radiation - Copper Kα
Data Set:
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.658 Å | (40) |
2.866 Å | (5) |
2.838 Å | (30) |
2.796 Å | (10) |
2.677 Å | (100) |
2.662 Å | (100) |
2.557 Å | (10) |
2.440 Å | (90) |
2.418 Å | (95) |
2.412 Å | (95) |
2.204 Å | (25) |
2.095 Å | (20) |
2.017 Å | (5) |
1.961 Å | (50) |
1.943 Å | (25) |
1.824 Å | (70) |
1.814 Å | (90) |
1.787 Å | (5) |
1.759 Å | (20) |
1.750 Å | (5) |
1.703 Å | (5) |
1.631 Å | (30) |
1.608 Å | (25) |
1.594 Å | (15) |
1.589 Å | (20) |
1.543 Å | (20) |
1.537 Å | (20) |
1.390 Å | (5) |
1.343 Å | (15) |
Comments:
ICDD 14-218 (Freiberg, Germany)
Geological EnvironmentHide
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Geological Setting:
High-temperature gold-quartz or tin hydrothermal veins, pegmatites, contact metamorphic rocks, gneisses, schists.
Synonyms of ArsenopyriteHide
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Other Language Names for ArsenopyriteHide
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Varieties of ArsenopyriteHide
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Argentiferous Mispickel | Name for a silver-bearing arsenopyrite.Needs reinvestigation because not confirmed in modern studies. |
---|---|
Danaite | A Co-bearing variety of arsenopyrite.Originally described from Franconia, Grafton Co., New Hampshire, USA.NB: Not to be confused with Danalite, a species in the helvine group. |
Relationship of Arsenopyrite to other SpeciesHide
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Other Members of Arsenopyrite Group:
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.EB. | Selenolaurite | RuSe2 | Iso. m_3(2/m_3) : P _a_3 |
---|---|---|---|
2.EB. | Andrieslombaardite | RhSbS | Iso. 23 : _P_213 |
2.EB. | Iridarsenite | (Ir,Ru)As2 | Mon. 2/m : _P_21/b |
2.EB. | Kanatzidisite | (SbBiS3)2Te2 | Mon. 2/m : _P_21/m |
2.EB.05a | Vaesite | NiS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Hauerite | MnS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Laurite | RuS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Gaotaiite | Ir3Te8 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Penroseite | (Ni,Co,Cu)Se2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Fukuchilite | Cu3FeS8 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Villamanínite | (Cu,Ni,Co,Fe)S2 | Tric. |
2.EB.05a | Erlichmanite | OsS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Sperrylite | PtAs2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Geversite | PtSb2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Cattierite | CoS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Aurostibite | AuSb2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Trogtalite | CoSe2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a v | Cayeuxite | ||
2.EB.05a | Kruťaite | CuSe2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Pyrite | FeS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Insizwaite | Pt(Bi,Sb)2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05b | Bambollaite | Cu(Se,Te)2 | Tet. |
2.EB.05a | Dzharkenite | FeSe2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.10a | Marcasite | FeS2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10e | Paracostibite | CoSbS | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
2.EB.10f | Oenite | CoSbAs | Orth. |
2.EB.10e | Pararammelsbergite | NiAs2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
2.EB.10a | Mattagamite | CoTe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10a | Frohbergite | FeTe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10d | Costibite | CoSbS | Orth. m _m_2 : P m _n_21 |
2.EB.10b | Alloclasite | Co1-xFexAsS | Mon. 2 : _P_21 |
2.EB.10c | Glaucodot | (Co0.50Fe0.50)AsS | Orth. m _m_2 : P m _n_21 |
2.EB.10a | Petříčekite | CuSe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10a | Kullerudite | NiSe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10a | Ferroselite | FeSe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15b | Seinäjokite | FeSb2 | Orth. |
2.EB.15a | Rammelsbergite | NiAs2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Clinosafflorite | CoAs2 | Mon. 2/m : _P_21/m |
2.EB.15c | Paxite | CuAs2 | Mon. 2/m : _P_21/b |
2.EB.15a | Nisbite | NiSb2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Löllingite | FeAs2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Safflorite | (Co,Ni,Fe)As2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Omeiite | (Os,Ru)As2 | Orth. |
2.EB.15a | Anduoite | (Ru,Os)As2 | Orth. |
2.EB.20 | Ruarsite | (Ru,Os)AsS | Mon. |
2.EB.20 | Osarsite | (Os,Ru)AsS | Mon. |
2.EB.20 | Gudmundite | FeSbS | Mon. 2/m : _P_21/b |
2.EB.25 | Mayingite | IrBiTe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Maslovite | PtBiTe | Iso. 23 : _P_213 |
2.EB.25 | Paragersdorffite | Ni(As,S)2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Orthogersdorffite | NiAsS | Orth. m _m_2 : P c _a_21 |
2.EB.25 | Jolliffeite | NiAsSe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Cobaltite | CoAsS | Orth. m _m_2 : P c _a_21 |
2.EB.25 | Testibiopalladite | PdSbTe | Iso. |
2.EB.25 va | Antimony-bearing Gersdorffite | Ni(As,Sb)S | |
2.EB.25 | Kalungaite | PdAsSe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Hollingworthite | (Rh,Pt,Pd)AsS | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Michenerite | PdBiTe | Iso. 23 : _P_213 |
2.EB.25 | Gersdorffite | NiAsS | Iso. 23 : _P_213 |
2.EB.25 | Milotaite | PdSbSe | Iso. 23 : _P_213 |
2.EB.25 | Tolovkite | IrSbS | Iso. |
2.EB.25 | Platarsite | Pt(As,S)2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Willyamite | CoSbS | |
2.EB.25 | Changchengite | IrBiS | Iso. 23 : _P_213 |
2.EB.25 | Kvačekite | NiSbSe | Iso. 23 : _P_213 |
2.EB.25 | Krutovite | NiAs2 | Iso. 23 : _P_213 |
2.EB.25 | Padmaite | PdBiSe | Iso. 432 |
2.EB.25 | Ullmannite | NiSbS | Iso. 23 : _P_213 |
2.EB.25 | Irarsite | (Ir,Ru,Rh,Pt)AsS | Iso. m_3(2/m_3) : P _a_3 |
2.EB.30 | Urvantsevite | Pd(Bi,Pb)2 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_4/m m m |
2.EB.35 | Rheniite | ReS2 | Tric. 1 : _P_1 |
Fluorescence of ArsenopyriteHide
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Other InformationHide
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Notes:
Decomposed by nitric acid with separation of arsenous acid and sulphur.
In a closed tube, at first gives a red sublimate of arsenic sulfide, then a black lustrous sublimate of metallic arsenic. In an open tube, gives sulphurous fumes and a white sublimate of arsenous acid.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Arsenopyrite in petrologyHide
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An essential component of rock names highlighted in red, an accessory component in rock names highlighted in green.
Internet Links for ArsenopyriteHide
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References for ArsenopyriteHide
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Reference List:
Brostigen, G., Kjekshus, A., Rømming, Chr., Gronowitz, Salo, Koskikallio, Jouko, Swahn, Carl-Gunnar (1973) Compounds with the Marcasite Type Crystal Structure. VIII. Redetermination of the Prototype. Acta Chemica Scandinavica, 27. 2791-2796 doi:10.3891/acta.chem.scand.27-2791
Schaufuss, Andrea G., Nesbitt, H. Wayne, Scaini, Michael J., Hoechst, Hartmut, Bancroft, Michael G., Szargan, Rüdiger (2000) Reactivity of surface sites on fractured arsenopyrite (FeAsS) toward oxygen. American Mineralogist, 85 (11) 1754-1766 doi:10.2138/am-2000-11-1219
Bindi, L., Moëlo, Y., Leone, P., Suchaud, M. (2012) Stoichiometric arsenopyrite, FeAsS, from La Roche-Balue Quarry, Loire-Atlantique, France: Crystal structure and Mössbauer study. The Canadian Mineralogist, 50 (2). 471-479 doi:10.3749/canmin.50.2.471
Fougerouse, Denis, Reddy, Steven M., Saxey, David W., Rickard, William D.A., van Riessen, Arie, Micklethwaite, Steven (2016) Nanoscale gold clusters in arsenopyrite controlled by growth rate not concentration: Evidence from atom probe microscopy. American Mineralogist, 101 (8) 1916-1919 doi:10.2138/am-2016-5781ccbyncnd
Significant localities for ArsenopyriteHide
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Showing 26 significant localities out of 11,125 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
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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.