Jacutingaite (original) (raw)
A valid IMA mineral species
About JacutingaiteHide
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Name:
The mineral is named after the specular-hematite-rich vein-type mineralization locally known as “jacutinga”, in which it occurs.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:41903:7
332de965-35c7-440e-9ba4-d3a4e33783eb
IMA Classification of JacutingaiteHide
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Type description reference:
Vymazalova, A., Laufek, F., Drabek, M., Cabral, A. R., Haloda, J., Sidorinova, T., Lehmann, B., Galbiatti, H. F., Drahokoupil, J. (2012) JACUTINGAITE, Pt2HgSe3, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE CAUE IRON-ORE DEPOSIT, ITABIRA DISTRICT, MINAS GERAIS, BRAZIL. The Canadian Mineralogist, 50 (2) 431-440 doi:10.3749/canmin.50.2.431
Classification of JacutingaiteHide
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2.CC.45
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
C : Metal Sulfides, M: S = 1: 1 (and similar)
C : With Ni, Fe, Co, 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 |
---|---|---|
Jac | 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 JacutingaiteHide
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Hardness:
VHN10=169 kg/mm2 - Vickers
Comment:
On synthetic material
Optical Data of JacutingaiteHide
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Anisotropism:
Weak to distinct.
Bireflectance:
Moderate to distinct.
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
420nm | 45.6% | 50.0% |
440nm | 46.3% | 50.6% |
460nm | 47.1% | 51.0% |
470nm | 47.4% | 51.1% |
480nm | 47.7% | 51.1% |
500nm | 48.0% | 51.1% |
520nm | 48.2% | 50.8% |
540nm | 48.2% | 50.6% |
546nm | 48.2% | 50.5% |
560nm | 48.2% | 50.3% |
580nm | 48.1% | 49.9% |
589nm | 48.0% | 49.6% |
600nm | 47.9% | 49.3% |
620nm | 47.7% | 48.8% |
640nm | 47.3% | 48.1% |
650nm | 47.1% | 47.8% |
660nm | 46.8% | 47.5% |
680nm | 46.3% | 46.9% |
700nm | 45.7% | 46.2% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 51.1%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Light grey.
Internal Reflections:
None.
Comments:
Bluish grey to rusty brown.
Chemistry of JacutingaiteHide
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Crystallography of JacutingaiteHide
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Class (H-M):
3_m_ _(_32/m ) - Hexagonal Scalenohedral
Cell Parameters:
a = 7.3477(2) Å, c = 5.2955(1) Å
Unit Cell V:
247.59 ų (Calculated from Unit Cell)
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
5.292 Å | (100) |
2.727 Å | (16) |
2.444 Å | (10) |
2.035 Å | (18) |
1.765 Å | (37) |
1.324 Å | (11) |
1.045 Å | (11) |
Geological EnvironmentHide
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Type Occurrence of JacutingaiteHide
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General Appearance of Type Material:
Place of Conservation of Type Material:
GeoMuseum, Technical University of Clausthal, Germany, cat. no. 26580.
Geological Setting of Type Material:
iron ore deposit specular-hematite-rich vein-type mineralization
Associated Minerals at Type Locality:
Reference:
Vymazalová, A., Laufek, F., Drábek, M., Cabral, A.R., Haloda, J., Sidorinová, T., Lehmann, B., Galbiatti, H.F., Drahokoupil, J. (2012) Jacutingaite, Pt2HgSe3, a new platinum-group mineral species from the Cauê iron-ore deposit, Itabira district, Minas Gerais, Brazil. The Canadian Mineralogist: 50(2): 431-440.
Synonyms of JacutingaiteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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2.CC. | Tilkerodeite | Pd2HgSe3 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
---|---|---|---|
2.CC. | UM2007-26-S:CuFeIrNiPtRh | (Ir,Cu,Ni,Pt,Rh,Fe)9S11 | |
2.CC. | Crowningshieldite | (Ni0.9Fe0.1)S | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC. | Eliopoulosite | V7S8 | Trig. 32 : _P_3221 |
2.CC. | Kuvaevite | Ir5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Torryweiserite | Rh5Ni10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Tamuraite | Ir5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC. | Ferrotorryweiserite | Rh5Fe10S16 | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC.05 | Achávalite | FeSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Breithauptite | NiSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Freboldite | CoSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Kotulskite | Pd(Te,Bi)2-x (x ≈ 0.4) | Hex. |
2.CC.05 | Langisite | CoAs | Hex. 6 : _P_63 |
2.CC.05 | Nickeline | NiAs | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m c m |
2.CC.05 | Sederholmite | beta-NiSe | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sobolevskite | PdBi | Hex. |
2.CC.05 | Stumpflite | PtSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Sudburyite | PdSb | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.05 | Jaipurite | CoS | Hex. |
2.CC.05 | Zlatogorite | NiCuSb2 | Trig. 3_m_ _(_32/m ) : P_31_m |
2.CC.10 | Pyrrhotite | Fe1-xS | Mon. |
2.CC.10 | Smythite | (Fe,Ni)3+xS4 (x=0-0.3) | Trig. 3_m_ _(_32/m ) : R_3_m |
2.CC.10 | Troilite | FeS | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.15 | Cherepanovite | RhAs | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.15 | Modderite | (Co,Fe)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Ruthenarsenite | (Ru,Ni)As | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.15 | Westerveldite | (Fe,Ni,Co)As | Orth. m m m _(_2/_m_2/_m_2/m ) |
2.CC.15 | Minakawaite | RhSb | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
2.CC.20 | Millerite | NiS | Trig. 3_m_ : R_3_m |
2.CC.20 | Mäkinenite | γ-NiSe | Trig. 3_m_ |
2.CC.20 | UM1990-38-S:CuFeIrNiPtRh | (Ni,Fe,Rh,Cu,Ir,Pt)S | |
2.CC.25 | Mackinawite | FeS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n m m |
2.CC.30 | Hexatestibiopanickelite | (Pd,Ni)(Sb,Te) ? | Hex. |
2.CC.30 | Vavřínite | Ni2SbTe2 | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
2.CC.35a | Braggite | PdPt3S4 | Tet. 4/m : _P_42/m |
2.CC.35b | Cooperite | PtS | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_42/m m c |
2.CC.35a | Vysotskite | PdS | Tet. 4/m : _P_42/m |
2.CC.50 | Imgreite | NiTe (?) | Hex. |
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 JacutingaiteHide
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References for JacutingaiteHide
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Reference List:
Cabral, A. R., Galbiatti, H. F., Kwitko-Ribeiro, R., Lehmann, B. (2008) Platinum enrichment at low temperatures and related microstructures, with examples of hongshiite (PtCu) and empirical ‘Pt2HgSe3’ from Itabira, Minas Gerais, Brazil. Terra Nova, 20 (1). 32-37 doi:10.1111/j.1365-3121.2007.00783.x
Vymazalova, A., Laufek, F., Drabek, M., Cabral, A. R., Haloda, J., Sidorinova, T., Lehmann, B., Galbiatti, H. F., Drahokoupil, J. (2012) JACUTINGAITE, Pt2HgSe3, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE CAUE IRON-ORE DEPOSIT, ITABIRA DISTRICT, MINAS GERAIS, BRAZIL. The Canadian Mineralogist, 50 (2) 431-440 doi:10.3749/canmin.50.2.431
Vymazalova, A., Laufek, F., Drabek, M., Cabral, A. R., Haloda, J., Sidorinova, T., Lehmann, B., Galbiatti, H. F., Drahokoupil, J. (2012) JACUTINGAITE, Pt2HgSe3, A NEW PLATINUM-GROUP MINERAL SPECIES FROM THE CAUE IRON-ORE DEPOSIT, ITABIRA DISTRICT, MINAS GERAIS, BRAZIL. The Canadian Mineralogist, 50 (2) 431-440 doi:10.3749/canmin.50.2.431
Longuinhos, Raphael, Vymazalová, Anna, Cabral, Alexandre R., Alexandre, Simone S., Nunes, Ricardo W., Ribeiro‐Soares, Jenaina (2020) Raman spectrum of layered jacutingaite (Pt 2 HgSe 3 ) crystals—Experimental and theoretical study. Journal of Raman Spectroscopy, 51 (2). 357-365 doi:10.1002/jrs.5764
Localities for JacutingaiteHide
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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.
Brazil (TL) | |
---|---|
Minas Gerais Itabira ⓘ Cauê mine (TL) | Cabral et al. (2008) +2 other references |
Serro ⓘ Córrego Bom Sucesso placers | Cabral et al. (2021) |
Czech Republic | |
Liberec Region Semily District Košťálov ⓘ |
Malec J. et al.: Jacutingait (podkrkonošská pánev) |
Germany | |
Saxony-Anhalt Mansfeld-Südharz Mansfeld Tilkerode Mining District ⓘ Eskaborn adit | Ma et al. (2020) |