Paracostibite (original) (raw)
A valid IMA mineral species
Colour:
White with a faint grayish tinge
Specific Gravity:
6.9 - 6.97
Crystal System:
Orthorhombic
Name:
Named from the Greek 'para' for near, and costibite, for the polymorphic relationship to that mineral.
Appears to be the high-temperature polymorph of CoSbS (Cabri et al., 1970).
Compare willyamite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3085:0
24bdbdf2-b3d3-4665-af85-64aecaf6544a
IMA Classification of ParacostibiteHide
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Type description reference:
Classification of ParacostibiteHide
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2.EB.10e
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.
2.12.7.2
2 : SULFIDES
12 : AmBnXp, with (m+n):p = 1:2
3.10.14
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.
Symbol | Source | Reference |
---|---|---|
Pcsb | 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 ParacostibiteHide
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Colour:
White with a faint grayish tinge
Hardness:
VHN15=936 - 1031 kg/mm2 - Vickers
Density:
6.9 - 6.97 g/cm3 (Measured)
Optical Data of ParacostibiteHide
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Bireflectance:
Weak, white in colour with a faint greyish tinge
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
470nm | 47.8% | 46.9% |
546nm | 48.1% | 47.5% |
589nm | 48.4% | 47.7% |
650nm | 48.8% | 48.0% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 48.8%.
R1 shown in black, R2 shown in red
Chemistry of ParacostibiteHide
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Common Impurities:
Fe,Ni,As
Crystallography of ParacostibiteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 5.76 Å, b = 5.94 Å, c = 11.66 Å
Ratio:
a:b:c = 0.97 : 1 : 1.963
Unit Cell V:
398.94 ų (Calculated from Unit Cell)
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0005115 | Paracostibite | Rowland J F, Gabe E J, Hall S R (1975) The crystal structures of costibite (CoSbS) and paracostibite(CoSbS) The Canadian Mineralogist 13 188-196 | 1975 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.555 Å | (10) |
2.035 Å | (8) |
5.81 Å | (8) |
1.853 Å | (8) |
2.826 Å | (7) |
2.654 Å | (7) |
2.976 Å | (4) |
Geological EnvironmentHide
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Type Occurrence of ParacostibiteHide
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General Appearance of Type Material:
Irregular and subhedral grains up to about 130 microns.
Place of Conservation of Type Material:
National Mineral Collection, Ottawa, Ontario, Canada.
Royal Ontario Museum, Toronto, Ontario, Canada.
Associated Minerals at Type Locality:
Reference:
Cabri, L.J., Harris, D.C., Stewart, J.M. (1970) Paracostibite (CoSbS) and nisbite (NiSb2), new minerals from the Red Lake Area, Ontario, Canada. The Canadian Mineralogist: 10: 232–246.
Synonyms of ParacostibiteHide
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Other Language Names for ParacostibiteHide
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Relationship of Paracostibite 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.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 | 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 | (Fe,Ni)(Sb,As)2 | 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 ParacostibiteHide
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References for ParacostibiteHide
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Reference List:
Zakrzewski, M.A., Burke, E.A.J., Nugteren, H.W. (1980) Cobalt Minerals in the Hällefors area, Bergslagen, Sweden: New occurences of costibite, paracostibite, nisbite and cobaltian ullmannite. The Canadian Mineralogist, 18 (2) 165-171
Localities for ParacostibiteHide
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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.
Australia | |
---|---|
New South Wales Yancowinna Co. Broken Hill district ⓘ Broken Hill | Worner et al. (et al) |
ⓘ Consols Mine (ABH Consols Mine; Australian Broken Hill Consols Mine) | L.Lawrence +1 other reference |
Austria | |
Salzburg Zell am See District Bramberg am Wildkogel Nasenkopf mountain ⓘ Greinerrinne | Taucher J. (1996) |
Canada (TL) | |
Ontario Kenora District Mulcahy Township ⓘ Trout Bay Copper Mine (TL) | Cabri et al. (1970) |
Japan | |
Iwate Prefecture Kamaishi City ⓘ Kamaishi mine ? | Ichikawa and Matsueda (1980) |
Russia | |
Primorsky Krai Dalnerechensky District Malinovsky cluster ⓘ Malinovka deposit | Gvozdev et al. (2016) |
Sweden | |
Örebro County Askersund Hammar ⓘ |
Zakrzewski et al. (1986) |
Hällefors Grythyttan ⓘ Björskogsnäs | Burke et al. (1990) |
Värmland County Filipstad Persberg ore district Getön ⓘ Getön Silver Mine | |
Gruvåsen mines ⓘ Lång Mines | Zakrzewski et al. (1980) |
UK | |
England Cornwall St Just Botallack Botallack Mine ⓘ Wheal Cock ? | Golley et al. (1995) |