Oenite (original) (raw)
A valid IMA mineral species
Specific Gravity:
7.91 (Calculated)
Crystal System:
Orthorhombic
Name:
Named after Oen Ing Soen (30 June 1928, Semarang, Indonesia (then Dutch East Indies) - 14 October 1996, Amsterdam, Netherlands), Professor of Petrology, Mineralogy and Ore Geology at the University of Amsterdam and the Free University in Amsterdam.
This page provides mineralogical data about Oenite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:7201:0
1c460f16-ca03-4157-94cd-71c985ad59d8
IMA Classification of OeniteHide
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Type description reference:
Classification of OeniteHide
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2.EB.10f
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.
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 |
|---|---|---|
| Oen | 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 OeniteHide
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Hardness:
VHN100=599 kg/mm2 - Vickers
Fracture:
Irregular/Uneven
Density:
7.91 g/cm3 (Calculated)
Optical Data of OeniteHide
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Anisotropism:
Distinct, reddish brown to darker pale violet
Bireflectance:
None in air, weak in oil
Reflectivity:
| Wavelength | R1 | R2 |
|---|---|---|
| 470nm | 58.2% | 55.5% |
| 546nm | 56.8% | 55.6% |
| 589nm | 55.8% | 55.5% |
| 650nm | 55.0% | 55.5% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 58.2%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Silver white in air, creamy tint in oil
Comments:
None in air. Very weak in oil, white to slightly darker creamy white.
Chemistry of OeniteHide
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Crystallography of OeniteHide
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Crystal System:
Orthorhombic
Cell Parameters:
a = 3.304 Å, b = 6.092 Å, c = 10.258 Å
Ratio:
a:b:c = 0.542 : 1 : 1.684
Unit Cell V:
206.47 ų (Calculated from Unit Cell)
Comment:
Class : nd; Space Group: nd
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 2.63 Å | (100) |
| 1.942 Å | (100) |
| 2.53 Å | (80) |
| 1.1182 Å | (80) |
| 1.730 Å | (40) |
| 1.640 Å | (40) |
| 1.3963 Å | (40) |
Geological EnvironmentHide
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Type Occurrence of OeniteHide
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General Appearance of Type Material:
Up to 300 µm silver-white anhedral aggregates in chalcopyrite as replacements of cobaltite and lollingite.
Place of Conservation of Type Material:
Instituut voor Aardwetenschappen, Vrije Universiteit, Amsterdam.
Geological Setting of Type Material:
In arsenide rich chalcopyrite ore. Skarn.
Associated Minerals at Type Locality:
Reference:
Dobbe, R.T.M, Zakrzewski, M.A. (1998) Oenite, CoSbAs, a new mineral species from the Tunaberg Cu–Co–sulfide skarns, Bergslagen, Sweden. The Canadian Mineralogist: 36: 855-860.
Synonyms of OeniteHide
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Other Language Names for OeniteHide
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Relationship of Oenite to other SpeciesHide
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Other Members of this group:
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.10b | Alloclasite | Co1-xFexAsS | Mon. 2 : _P_21 |
| 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.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 OeniteHide
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References for OeniteHide
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Localities for OeniteHide
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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.
| Russia | |
|---|---|
| Krasnoyarsk Krai Maimecha and Kotui Rivers Basin ⓘ Maimechinskaya intrusion | Гриценко et al. (2021) |
| Sweden (TL) | |
| Södermanland County Nyköping Tunaberg ⓘ Tunaberg Cu-Co Ore Field (TL) | Dobbe et al. (1998) |