Rohaite
A valid IMA mineral species
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Formula:
(Tl,Pb,K)2Cu8.7Sb2S4
Colour:
Black
Lustre:
Metallic
Hardness:
3 - 3½
Crystal System:
Orthorhombic
Name:
Named after John Rose-Hansen (2 May 1937, Copenhagen, Denmark - 18 September 2015), professor of mineralogy, University of Copenhagen, Denmark.
This page provides mineralogical data about Rohaite.
Unique Identifiers
Mindat ID:
3439
Long-form identifier:
mindat:1:1:3439:1
GUID
(UUID V4):
(UUID V4):
f0d70c65-74d7-40dc-9390-a331f843ad89
IMA Classification of Rohaite
Approved
IMA Formula:
(Tl,Pb,K)2Cu8.7Sb2S4
First published:
1978
Classification of Rohaite
2.BD.35
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
D : With Hg, Tl
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
D : With Hg, Tl
3.7.16.1
3 : SULFOSALTS
7 : ø = 2
3 : SULFOSALTS
7 : ø = 2
5.5.14
5 : Sulphosalts - Sulpharsenites and Sulphobismuthites (those containing Sn, Ge,or V are in Section 6)
5 : Sulpharsenites etc. of Tl
5 : Sulphosalts - Sulpharsenites and Sulphobismuthites (those containing Sn, Ge,or V are in Section 6)
5 : Sulpharsenites etc. of Tl
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Roh | 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 Rohaite
Metallic
Transparency:
Opaque
Colour:
Black
Comment:
In reflected light, yellowish cream to dull bluish gray.
Hardness:
3 - 3½ on Mohs scale
Hardness Data:
Could not be measured
Tenacity:
Malleable
Optical Data of Rohaite
Anisotropism:
Strong, yellowish-cream to black
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
481nm | 24.5% | 32.0% |
546nm | 22.3% | 32.4% |
590nm | 21.8% | 32.0% |
650nm | 20.8% | 31.8% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 32.4%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Yellowish-cream to dull bluish-gray
Pleochroism:
Strong
Comments:
Strong in air and oil
Comments:
Optically positive
Chemistry of Rohaite
Mindat Formula:
(Tl,Pb,K)2Cu8.7Sb2S4
Common Impurities:
Pb,Fe
Crystallography of Rohaite
Crystal System:
Orthorhombic
Cell Parameters:
a = 7.602(2) Å, b = 3.801(2) Å, c = 20.986(8) Å
Ratio:
a:b:c = 2 : 1 : 5.521
Unit Cell V:
606.39 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Rarely as euhedral and subhedral crystals (to 0.5 mm); in patchy aggregates.
Comment:
Space group P222, Pmm2, or Pmmm.
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.800 Å | (90) |
3.078 Å | (100) |
2.393 Å | (100) |
1.902 Å | (90) |
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Near-surface Processes | |
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | |
High-𝑇 alteration and/or metamorphism | |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) |
Type Occurrence of Rohaite
General Appearance of Type Material:
Grains from 0.05-0.5 mm.
Place of Conservation of Type Material:
University of Copenhagen, Geological Museum, Copenhagen, Denmark, 1979.1212 (cotype).
Geological Setting of Type Material:
In a vein rich in analcime and sodalite in an alkalic intrusive.
Associated Minerals at Type Locality:
Reference:
Karup-Møller, S. (1978) Primary and secondary ore minerals associated with cuprostibite. Bulletin Grønlands Geologiske Undersøgelse, 126, 23-47.
Synonyms of Rohaite
Other Language Names for Rohaite
Related Minerals - Strunz-mindat Grouping
2.BD. | UM2004-33-S:AgCuHgSe | (Ag,Cu)8Hg3(S,Se)7 |
2.BD. | Vrančiceite | Cu10Hg3S8 |
2.BD.05 | Imiterite | Ag2HgS2 |
2.BD.10 | Gortdrumite | Cu24Fe2Hg9S23 |
2.BD.15 | Balkanite | Cu9Ag5HgS8 |
2.BD.15 | Danielsite | (Cu,Ag)14HgS8 |
2.BD.20 | Donharrisite | Ni3HgS3 |
2.BD.25 | Carlinite | Tl2S |
2.BD.30 | Bukovite | (Cu3Fe)Σ4Tl2Se4 |
2.BD.30 | Murunskite | K2(Cu,Fe)4S4 |
2.BD.30 | Thalcusite | Tl2Cu3FeS4 |
2.BD.40 | Chalcothallite | Tl2(Cu,Fe)6SbS4 |
2.BD.45 | Sabatierite | TlCu6Se4 |
2.BD.50 | Crookesite | Cu7(Tl, Ag)Se4 |
2.BD.55 | Brodtkorbite | Cu2HgSe2 |
Other Information
Notes:
Alters readily to a mixture of digenite and senarmontite.
Etch tests with HgCl2, KOH, KCN, and FeCl3 were negative. With HCl (1:1) the mineral turned slightly steel-bluish gray, with HNO3 (1:1) the polished surface is destroyed and the mineral turns black.
Etch tests with HgCl2, KOH, KCN, and FeCl3 were negative. With HCl (1:1) the mineral turned slightly steel-bluish gray, with HNO3 (1:1) the polished surface is destroyed and the mineral turns black.
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 Rohaite
mindat.org URL:
https://www.mindat.org/min-3439.html
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References for Rohaite
Reference List:
Localities for Rohaite
Locality List
- 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.
All localities listed without proper references should be considered as questionable.
Greenland | |
| American Mineralogist (1980) +1 other reference |
| Petersen et al. (2005) |
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