Schlemaite
A valid IMA mineral species
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About Schlemaite
Formula:
(Cu,◻)6(Pb,Bi)Se4
Colour:
Black
Lustre:
Metallic
Hardness:
3
Specific Gravity:
7.54 (Calculated)
Crystal System:
Monoclinic
Name:
For the type locality, in the Schlema-Hartenstein District (Niederschlema-Alberoda mining area), Erzgebirge, Saxony, Germany.
Type Locality:
This page provides mineralogical data about Schlemaite.
Unique Identifiers
Mindat ID:
25688
Long-form identifier:
mindat:1:1:25688:1
GUID
(UUID V4):
(UUID V4):
70c29815-4aec-4477-bff8-e62daaa31493
IMA Classification of Schlemaite
Classification of Schlemaite
2.BE.25
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
E : With Pb (Bi)
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
E : With Pb (Bi)
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 |
---|---|---|
Slm | 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 Schlemaite
Metallic
Transparency:
Opaque
Colour:
Black
Streak:
Black
Hardness:
3 on Mohs scale
Hardness:
VHN25=106 kg/mm2 - Vickers
Hardness Data:
Measured
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
7.54 g/cm3 (Calculated)
Optical Data of Schlemaite
Anisotropism:
Very weak, with rotation tints in shades of very pale metallic orange and blue
Bireflectance:
Very weak
Reflectivity:
Wavelength | R1 | R2 | imR1 | imR2 |
---|---|---|---|---|
400nm | 35.3% | 36.2% | 20.6% | 21.7% |
420nm | 36.1% | 37.1% | 20.9% | 22.3% |
440nm | 36.3% | 37.65% | 21.1% | 22.7% |
460nm | 36.3% | 38.0% | 21.1% | 23.0% |
470nm | 36.6% | 38.1% | 21.1% | 23.0% |
480nm | 36.6% | 38.1% | 21.05% | 23.1% |
500nm | 36.5% | 38.1% | 20.8% | 22.9% |
520nm | 36.4% | 38.1% | 20.7% | 22.8% |
540nm | 36.5% | 38.1% | 20.7% | 22.8% |
546nm | 36.45% | 38.1% | 20.7% | 22.8% |
560nm | 36.4% | 38.2% | 20.7% | 22.8% |
580nm | 36.55% | 38.2% | 20.9% | 22.9% |
589nm | 36.6% | 38.3% | 20.95% | 22.9% |
600nm | 36.7% | 38.35% | 21.0% | 23.1% |
620nm | 36.7% | 38.4% | 21.1% | 23.1% |
640nm | 36.7% | 38.5% | 21.0% | 23.2% |
650nm | 36.6% | 38.5% | 21.0% | 23.2% |
660nm | 36.6% | 38.4% | 21.1% | 23.2% |
680nm | 36.7% | 38.4% | 21.1% | 23.2% |
700nm | 36.4% | 38.5% | 21.0% | 23.4% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 38.5%.
R1 shown in black, R2 shown in red, imR1 shown in green, imR2 shown in blue
Colour in reflected light:
Grey
Internal Reflections:
None
Pleochroism:
Non-pleochroic
Chemistry of Schlemaite
Mindat Formula:
(Cu,◻)6(Pb,Bi)Se4
Elements listed:
Crystallography of Schlemaite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Cell Parameters:
a = 9.5341 Å, b = 4.1004 Å, c = 10.2546 Å
β = 100.066°
β = 100.066°
Ratio:
a:b:c = 2.325 : 1 : 2.501
Unit Cell V:
394.72 ų
Z:
2
Twinning:
None observed.
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.34 Å | (80) |
3.17 Å | (60) |
2.85 Å | (80) |
2.69 Å | (80) |
2.17 Å | (60) |
2.10 Å | (70) |
2.07 Å | (100) |
2.04 Å | (50) |
Comments:
From type description.
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
High-𝑇 alteration and/or metamorphism | |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) |
Type Occurrence of Schlemaite
General Appearance of Type Material:
Anhedral to subhedral grains, up to a few 100 µm in size.
Place of Conservation of Type Material:
The Natural History Museum, London, England (BM 2003,4).
Mineralogical Institute, Technische Universität Bergakademie, Freiberg, Germany (80824).
Mineralogical Institute, Technische Universität Bergakademie, Freiberg, Germany (80824).
Geological Setting of Type Material:
In hydrothermal Se-bearing dolomite-ankerite veins.
Associated Minerals at Type Locality:
Synonyms of Schlemaite
Other Language Names for Schlemaite
Common Associates
Associated Minerals Based on Photo Data:
1 photo of Schlemaite associated with Berzelianite | Cu2-xSe (x ≈ 0.12) |
1 photo of Schlemaite associated with Eucairite | AgCuSe |
1 photo of Schlemaite associated with Clausthalite | PbSe |
1 photo of Schlemaite associated with Ankerite-Dolomite Series |
Related Minerals - Strunz-mindat Grouping
2.BE. | Zipserite | Bi5S4 |
2.BE.05 | Betekhtinite | Pb2(Cu,Fe)22-24S15 |
2.BE.10 | Furutobeite | (Cu,Ag)6PbS4 |
2.BE.15 | Rhodplumsite | Rh3Pb2S2 |
2.BE.15 | Shandite | Ni3Pb2S2 |
2.BE.20 | Parkerite | Ni3(Bi,Pb)2S2 |
2.BE.30 | Pašavaite | Pd3Pb2Te2 |
Other Information
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 Schlemaite
mindat.org URL:
https://www.mindat.org/min-25688.html
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Please feel free to link to this page.
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External Links:
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References for Schlemaite
Reference List:
Forster, H.-J., Cooper, M. A., Roberts, A. C., Stanley, C. J., Criddle, A. J., Hawthorne, F. C., Laflamme, J.H. G., Tischendorf, G. (2003) Schlemaite, (Cu,◻)6(Pb,Bi)Se4, a new mineral species from Neiderschlema-Alberoda, Erzgebirge, Germany: description and crystal structure. The Canadian Mineralogist, 41 (6) 1433-1444 doi:10.2113/gscanmin.41.6.1433
Localities for Schlemaite
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.
Germany | |
| Forster et al. (2004) |
| Forster et al. (2003) |
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Shaft 371, Hartenstein, Zwickau District, Saxony, Germany