Zinkosite
A valid IMA mineral species - grandfathered - questionable
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Formula:
ZnSO4
Specific Gravity:
4.33
Crystal System:
Orthorhombic
Probably an artificial product, and its occurence in nature (at least at its "type locality") is doubtful (Calvo and Viñals, 2008).
Unique Identifiers
Mindat ID:
4418
Long-form identifier:
mindat:1:1:4418:5
Similar Names
| Native Zinc | A valid IMA mineral species - grandfathered | Zn |
| Sincosite | A valid IMA mineral species - grandfathered | Ca(V4+O)2(PO4)2 · 4H2O |
| Zincite | A valid IMA mineral species - grandfathered | ZnO |
| Zinkenite | A valid IMA mineral species - grandfathered | Pb9Sb22S42 |
IMA Classification of Zinkosite
Approved, 'Grandfathered' (first described prior to 1959), Questionable
IMA Formula:
Zn2+S6+O4
Classification of Zinkosite
7.AB.10
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
B : With medium-sized cations
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
B : With medium-sized cations
25.5.1
25 : Sulphates
5 : Sulphates of Zn and Hg
25 : Sulphates
5 : Sulphates of Zn and Hg
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 for Standard |
|---|---|---|
| Zin | 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 Zinkosite
Transparency:
Translucent
Density:
4.33 g/cm3 (Measured) 3.86 g/cm3 (Calculated)
Optical Data of Zinkosite
Type:
Biaxial (-)
RI values:
nα = 1.658 nβ = 1.669 nγ = 1.67
2V:
Measured: 25° , Calculated: 32°
Max. Birefringence:
δ = 0.012
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
strong
Chemistry of Zinkosite
Mindat Formula:
ZnSO4
Element Weights:
Elements listed:
Crystallography of Zinkosite
Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pnma
Setting:
Pnma
Cell Parameters:
a = 8.604(5) Å, b = 6.746(5) Å, c = 4.774(3) Å
Ratio:
a:b:c = 1.275 : 1 : 0.708
Unit Cell V:
277.10 ų (Calculated from Unit Cell)
Z:
4
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0014620 | Zinkosite | Wildner M, Giester G (1988) Crystal structure refinements of synthetic chalcocyanite (CuSO4) and zincosite (ZnSO4) Mineralogy and Petrology 39 201-209 | 1988 | synthetic | 0 | 293 | |
| 0009208 | Zinkosite | Kokkoros P A, Rentzeperis P J (1958) The crystal structure of the anhydrous sulphates of copper and zinc Acta Crystallographica 11 361-364 | ![]() | 1958 | 0 | 293 |
CIF Raw Data - click here to close
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47b : [Sulfates and sulfites] | |
| 47h : [Near-surface oxidized, dehydrated minerals] |
Type Occurrence of Zinkosite
Synonyms of Zinkosite
Other Language Names for Zinkosite
Dutch:Zinkosiet
German:Zinkosit
Almagrerit
Zincosit
Almagrerit
Zincosit
Russian:Цинкозит
Spanish:Almagrerita
Zincosita
Zinkosita
Zincosita
Zinkosita
Related Minerals - Strunz-mindat Grouping
| 7.AB. | Dravertite | CuMg(SO4)2 |
| 7.AB. | Andymcdonaldite | Fe2TeO6 |
| 7.AB. | Dagenaisite | Zn3Te6+O6 |
| 7.AB.05 | Mikasaite | Fe2(SO4)3 |
| 7.AB.05 | Millosevichite | Al2(SO4)3 |
| 7.AB.05 | Koryakite | NaKMg2Al2(SO4)6 |
| 7.AB.10 | Chalcocyanite | CuSO4 |
| 7.AB.15 | Hermannjahnite | CuZn(SO4)2 |
| 7.AB.25 | Ottoite | Pb2TeO5 |
| 7.AB.55 | Mcalpineite | Cu3(Te6+O6) |
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 Zinkosite
mindat.org URL:
https://www.mindat.org/min-4418.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Zinkosite
Reference List:
Larsen, Esper S. (1921) The microscopic determination of the nonopaque minerals. Bulletin 679. US Geological Survey doi:10.3133/b679 p.159
Localities for Zinkosite
Showing 6 localities.
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).
All localities listed without proper references should be considered as questionable.
China | |
| Zhongjing Lingnan Nonferrous Metals Data |
Spain (TL) | |
| AM 45 (1960) |
Tunisia | |
| Somrani et al. (2025) |
| Somrani et al. (2025) |
USA | |
| Northrop et al. (1996) |
| Northrop et al. (1996) |
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