Pararammelsbergite (original) (raw)
A valid IMA mineral species - grandfathered
About PararammelsbergiteHide
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Crystal System:
Orthorhombic
Name:
Named in 1940 by Martin Alfred Peacock and Alexander Stewart Dadson from the Greek παρά = beyond and rammelsbergite, because of its relationship to the root mineral.
Co-Type Localities:
ⓘ Hudson Bay Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
ⓘ Moose Horn Mine, James Township, Elk Lake area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
ⓘ Keeley-Frontier Mine, South Lorrain Township, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
The low-temperature polymorph of NiAs2.
The crystal structure is transitional between the marcasite and pyrite structures (Fleet, 1972).
Compare, e.g., the (now approved / redefined) dienerite.
Peacock (1940) gives a summary of the early history and confusion surrounding the identity and naming of the species.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3106:2
79561d48-9055-4fe9-a7f6-b46c7a0fbf2a
IMA Classification of PararammelsbergiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
Classification of PararammelsbergiteHide
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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.
2.12.5.1
2 : SULFIDES
12 : AmBnXp, with (m+n):p = 1:2
3.11.29
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
11 : Sulphides etc. of Ni
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 |
---|---|---|
Prmb | 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 PararammelsbergiteHide
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Hardness:
VHN100=681 - 830 kg/mm2 - Vickers
Density:
7.12 g/cm3 (Measured) 7.24 g/cm3 (Calculated)
Optical Data of PararammelsbergiteHide
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Anisotropism:
Strong, in russet-brown, brown, yellow, gray.
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400nm | 57.3% | 57.7% |
420nm | 57.7% | 57.9% |
440nm | 58.1% | 58.1% |
460nm | 58.6% | 58.4% |
480nm | 58.9% | 58.7% |
500nm | 59.1% | 59.0% |
520nm | 59.1% | 59.2% |
540nm | 59.0% | 59.6% |
560nm | 58.8% | 60.0% |
580nm | 58.7% | 60.4% |
600nm | 58.5% | 60.7% |
620nm | 58.2% | 60.9% |
640nm | 58.0% | 61.1% |
660nm | 57.8% | 61.2% |
680nm | 57.6% | 61.3% |
700nm | 57.4% | 61.3% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 61.3%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Pure white
Chemistry of PararammelsbergiteHide
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Common Impurities:
Co,Cu,S
Crystallography of PararammelsbergiteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 5.753(6) Å, b = 5.799(6) Å, c = 11.407(9) Å
Ratio:
a:b:c = 0.992 : 1 : 1.967
Unit Cell V:
380.56 ų (Calculated from Unit Cell)
Comment:
From Fleet (1972).
Crystallographic forms of PararammelsbergiteHide
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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) |
---|---|---|---|---|---|---|---|
0000267 | Pararammelsbergite | Fleet M E (1972) The crystal structure of pararammelsbergite (NiAs2) American Mineralogist 57 1-9 | 1972 | 0 | 293 | ||
0012153 | Pararammelsbergite | Stassen W N, Heyding R D (1968) Crystal structures of RuSe2, OsSe2, PtAs2, and alpha-NiAs2 Canadian Journal of Chemistry 46 2159-2163 | 1968 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.855 Å | (50) |
2.827 Å | (48) |
2.602 Å | (45) |
2.559 Å | (100) |
2.541 Å | (45) |
2.521 Å | (96) |
2.371 Å | (67) |
2.337 Å | (67) |
1.821 Å | (52) |
1.741 Å | (66) |
1.533 Å | (45) |
1.380 Å | (45) |
Comments:
Synthetic. The data are from Bennett and Heyding (1966).
Geological EnvironmentHide
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Type Occurrence of PararammelsbergiteHide
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Co-Type Localities:
ⓘ Hudson Bay Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
ⓘ Moose Horn Mine, James Township, Elk Lake area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
ⓘ Keeley-Frontier Mine, South Lorrain Township, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada
General Appearance of Type Material:
Massive, in part minutely crystallized.
Place of Conservation of Type Material:
Royal Ontario Museum, Toronto, Ontario, Canada, numbers M11772a-c, M14242, and M12411 (cotype).
Other Language Names for PararammelsbergiteHide
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Relationship of Pararammelsbergite 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 | Paracostibite | CoSbS | 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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Notes:
Etch reactions:
HNO3, effervesces and etches rapidly brown to black.
FeCl, etches quickly light to dark brown, bringing out the texture.
HgCl2, slowly gives a brown to iridescent stain which does not rub off.
HCl, KCN, KOH, negative.
In air saturated with water vapour etching is already perceptible after four hours; in twelve hours the surface is deeply etched; after a week white and green bloom are formed. Pararammelsbergite appears to decompose more rapidly than rammelsbergite in moist air.
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 PararammelsbergiteHide
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References for PararammelsbergiteHide
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Localities for PararammelsbergiteHide
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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.