Alloclasite (original) (raw)
A valid IMA mineral species - grandfathered
About AlloclasiteHide
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Colour:
Steel gray to silver
Crystal System:
Monoclinic
Name:
For the Greek άλλος ("allos") for "other" and κλάσις ("klasis"), "to break", because its cleavage was believed to be different from marcasite.
See also the chemically very similar Cobaltite and Glaucodot. Compare 'UM1966-01-As:CoNiS'.
Fe content is distinctly higher than that of cobaltite, and the Fe usually occupies about 25% of the (Co,Fe) site (Kingston, 1971).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:134:2
8b2595eb-635e-4d0d-ad1b-89c8b48dc8f2
IMA Classification of AlloclasiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
Type description reference:
Classification of AlloclasiteHide
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2.EB.10b
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.
2.12.6.2
2 : SULFIDES
12 : AmBnXp, with (m+n):p = 1:2
3.10.16
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
10 : Sulphides etc. of Co
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 |
---|---|---|
Acl | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Alo | 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 AlloclasiteHide
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Colour:
Steel gray to silver
Hardness:
VHN100=818 - 940 kg/mm2 - Vickers
Cleavage:
Perfect
perfect on {101}
distinct on {010}
Fracture:
Irregular/Uneven, Sub-Conchoidal
Density:
5.95 g/cm3 (Measured) 6.188 g/cm3 (Calculated)
Optical Data of AlloclasiteHide
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Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 49.5% | 48.2% |
420nm | 48.7% | 48.3% |
440nm | 48.2% | 48.6% |
460nm | 47.8% | 48.8% |
480nm | 47.6% | 49.2% |
500nm | 47.6% | 49.7% |
520nm | 47.8% | 50.1% |
540nm | 48.0% | 50.4% |
560nm | 48.1% | 50.5% |
580nm | 48.4% | 50.6% |
600nm | 48.6% | 50.7% |
620nm | 48.8% | 50.7% |
640nm | 49.0% | 50.5% |
660nm | 49.1% | 50.3% |
680nm | 49.1% | 50.1% |
700nm | 49.2% | 49.9% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 50.7%.
R1 shown in black, R2 shown in red
Chemistry of AlloclasiteHide
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Crystallography of AlloclasiteHide
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Crystal System:
Monoclinic
Class (H-M):
2 - Sphenoidal
Cell Parameters:
a = 4.661 Å, b = 5.602 Å, c = 3.411 Å
β = 90.03°
Ratio:
a:b:c = 0.832 : 1 : 0.609
Unit Cell V:
89.06 ų (Calculated from Unit Cell)
Morphology:
Crystals are prismatic parallel [010] , to 5 mm, in columnar to radiating aggregates; commonly massive.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0005134 | Alloclasite | Scott J D, Nowacki W (1976) The crystal structure of alloclasite, CoAsS, and the alloclasite-cobaltite transformation The Canadian Mineralogist 14 561-566 | 1976 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.58 Å | (30) |
2.802 Å | (30) |
2.750 Å | (100) |
2.469 Å | (90) |
2.401 Å | (50) |
1.817 Å | (70) |
1.707 Å | (30) |
Geological EnvironmentHide
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Geological Setting:
In calcite or quartz veins of apparently low-temperature, late-stage hydrothermal origin. Also in silicified, recrystallized metamorphic rock.
Type Occurrence of AlloclasiteHide
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General Appearance of Type Material:
Place of Conservation of Type Material:
Reference:
Tschermak, G. (1866) Der alloklas und der sogenannte glaukodot von Orawicza. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften, 53, 220-225.
Synonyms of AlloclasiteHide
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Other Language Names for AlloclasiteHide
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Relationship of Alloclasite to other SpeciesHide
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Other Members of this group:
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.EB. | Iridarsenite | (Ir,Ru)As2 | Mon. 2/m : _P_21/b |
---|---|---|---|
2.EB. | Selenolaurite | RuSe2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB. | Andrieslombaardite | RhSbS | Iso. 23 : _P_213 |
2.EB. | Kanatzidisite | (SbBiS3)2Te2 | Mon. 2/m : _P_21/m |
2.EB.05a | Aurostibite | AuSb2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05b | Bambollaite | Cu(Se,Te)2 | Tet. |
2.EB.05a | Cattierite | CoS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Erlichmanite | OsS2 | 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 | Geversite | PtSb2 | 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 | Insizwaite | Pt(Bi,Sb)2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Krut'aite | CuSe2 | 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 | Penroseite | (Ni,Co,Cu)Se2 | 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 | Sperrylite | PtAs2 | 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 | Vaesite | NiS2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.05a | Villamanínite | (Cu,Ni,Co,Fe)S2 | Tric. |
2.EB.05a | Dzharkenite | FeSe2 | 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 v | Cayeuxite | ||
2.EB.10d | Costibite | CoSbS | Orth. m _m_2 : P m _n_21 |
2.EB.10a | Ferroselite | FeSe2 | 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.10c | Glaucodot | (Co0.50Fe0.50)AsS | Orth. m _m_2 : P m _n_21 |
2.EB.10a | Kullerudite | NiSe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10a | Marcasite | FeS2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.10a | Mattagamite | CoTe2 | 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.10e | Pararammelsbergite | NiAs2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
2.EB.10f | Oenite | CoSbAs | Orth. |
2.EB.10a | Petříčekite | CuSe2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Anduoite | (Ru,Os)As2 | Orth. |
2.EB.15a | Clinosafflorite | CoAs2 | Mon. 2/m : _P_21/m |
2.EB.15a | Löllingite | FeAs2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Nisbite | NiSb2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
2.EB.15a | Omeiite | (Os,Ru)As2 | Orth. |
2.EB.15c | Paxite | CuAs2 | Mon. 2/m : _P_21/b |
2.EB.15a | Rammelsbergite | NiAs2 | 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.15b | Seinäjokite | FeSb2 | Orth. |
2.EB.20 | Arsenopyrite | FeAsS | Mon. 2/m : _P_21/b |
2.EB.20 | Gudmundite | FeSbS | Mon. 2/m : _P_21/b |
2.EB.20 | Osarsite | (Os,Ru)AsS | Mon. |
2.EB.20 | Ruarsite | (Ru,Os)AsS | Mon. |
2.EB.25 va | Antimony-bearing Gersdorffite | Ni(As,Sb)S | |
2.EB.25 | Cobaltite | CoAsS | Orth. m _m_2 : P c _a_21 |
2.EB.25 | Gersdorffite | NiAsS | 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 | Irarsite | (Ir,Ru,Rh,Pt)AsS | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Jolliffeite | NiAsSe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Krutovite | NiAs2 | Iso. 23 : _P_213 |
2.EB.25 | Maslovite | PtBiTe | Iso. 23 : _P_213 |
2.EB.25 | Michenerite | PdBiTe | Iso. 23 : _P_213 |
2.EB.25 | Padmaite | PdBiSe | Iso. 432 |
2.EB.25 | Platarsite | Pt(As,S)2 | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Testibiopalladite | PdSbTe | Iso. |
2.EB.25 | Tolovkite | IrSbS | Iso. |
2.EB.25 | Ullmannite | NiSbS | Iso. 23 : _P_213 |
2.EB.25 | Willyamite | CoSbS | |
2.EB.25 | Changchengite | IrBiS | Iso. 23 : _P_213 |
2.EB.25 | Mayingite | IrBiTe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Kalungaite | PdAsSe | Iso. m_3(2/m_3) : P _a_3 |
2.EB.25 | Milotaite | PdSbSe | 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 | Kvačekite | NiSbSe | Iso. 23 : _P_213 |
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 |
Other InformationHide
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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 AlloclasiteHide
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References for AlloclasiteHide
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Localities for AlloclasiteHide
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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.