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Chromatite

A valid IMA mineral species
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About ChromatiteHide

Formula:
CaCr6+O4
Colour:
Yellow, violet
Lustre:
Dull, Earthy
Specific Gravity:
3.142 (Calculated)
Crystal System:
Tetragonal
Name:
Named by F. J. Eckhardt and W. Heimbach in 1963 for the chemical composition.
Earthy yellow coatings.

Isotypic with zircon and xenotime.

Compare 'UM2011-01-CrO:CaH' - a dihydrate counterpart; and the compositionally similar 'Unnamed (Calcium Chromium Oxide Postspinel)'. Also chemically similar to ellinaite.


Unique IdentifiersHide

Mindat ID:
1030
Long-form identifier:
mindat:1:1:1030:2

Similar NamesHide

AchromatiteA synonym of 'Achrematite'
ChromititeA rock classification type

IMA Classification of ChromatiteHide

Approved

Classification of ChromatiteHide

7.FA.10

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
F : Chromates
A : Without additional anions
Dana 7th ed.:
35.3.2.1
35.3.2.1

35 : ANHYDROUS CHROMATES
3 : AXO4
27.2.3

27 : Sulphites, Chromates, Molybdates and Tungstates
2 : Chromates

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
CrmIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Pronunciation of ChromatiteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of ChromatiteHide

Dull, Earthy
Transparency:
Translucent
Comment:
Low luster reported because of the powdery occurrence
Colour:
Yellow, violet
Comment:
Violet crystals (Mo-, Pb-bearing) from Bleiberg, Austria.
Streak:
Yellow
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
3.142 g/cm3 (Calculated)

Optical Data of ChromatiteHide

Type:
Uniaxial (+)
RI values:
nω = 1.81 - 1.85 nε = 1.84 - 1.88
Max. Birefringence:
δ = 0.030
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.

Surface Relief:
Very High (positive)
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.

Chemistry of ChromatiteHide

Mindat Formula:
CaCr6+O4
Element Weights:
Element% weight
O41.005 %
Cr33.316 %
Ca25.679 %

Calculated from ideal end-member formula.
O
Cr
Ca

Crystallography of ChromatiteHide

Crystal System:
Tetragonal
Class (H-M):
4/mmm(4/m2/m2/m) - Ditetragonal Dipyramidal
Space Group:
I41/amd
Cell Parameters:
a = 7.242 Å, c = 6.290 Å
Ratio:
a:c = 1 : 0.869
Unit Cell V:
329.89 ų (Calculated from Unit Cell)
Morphology:
Observed as earthy coating at type locality

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0017660ChromatiteClouse J (1932) Investigations on the X-Ray Crystal Structures of Ca Cr O4, Ca Cr O4 * H2 O and Ca Cr O4 * (H2 O)2 _cod_database_code 1010939 Zeitschrift fur Kristallographie 83 161-17119320293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.62 Å(100)
2.88 Å(20)
2.68 Å(50)
2.56 Å(10)
2.38 Å(20)
1.85 Å(40)
1.81 Å(20)
1.50 Å(10)
Comments:
8-458 synthetic

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
51 : Pyrometamorphic minerals (see also #54 and #56)<0.36

Type Occurrence of ChromatiteHide

General Appearance of Type Material:
Earthy coatings
Geological Setting of Type Material:
In sedimentary rock units at the type location.
Associated Minerals at Type Locality:

Other Language Names for ChromatiteHide

German:Chromatit
Spanish:Cromatita

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Chromatite associated with HalotrichiteFe2+Al2(SO4)4 · 22H2O

Related Minerals - Strunz-mindat GroupingHide

7.FA.05TarapacáiteK2(CrO4)Orth. mmm(2/m2/m2/m)
7.FA.15HashemiteBaCr6+O4Orth. mmm(2/m2/m2/m) : Pnma
7.FA.20CrocoitePbCr6+O4Mon. 2/m

Other InformationHide

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 ChromatiteHide

References for ChromatiteHide

Localities for ChromatiteHide

Showing 10 localities.

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.
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Locality ListHide

- 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.
Austria
 
  • Carinthia
    • Villach-Land District
      • Bad Bleiberg
Puttner (1997)
Greece
 
  • Central Macedonia
    • Imathia
Tsoupas et al. (2021)
Israel
 
  • Southern District
    • Beersheba Subdistrict
      • Tamar Regional Council
Gross (1977)
Jordan
 
  • Amman Governorate
    • Transjordan Plateau
      • Daba-Siwaqa complex
        • Hashem region
          • Lisdan-Siwaga Fault
            • Siwaga
              • Tulul al Hammam
Sokol +9 other references
Middle East
 
Gross (1977)
Norway
 
  • Telemark
    • Porsgrunn
      • Bjørkedalen
Piilonen et al. (2012) +1 other reference
Palestine
 
  • West Bank
    • Jericho Governorate
Sokol et al. (2011)
    • Quds Governorate
Naturwiss. (1963) +1 other reference
Russia
 
  • Sverdlovsk Oblast
    • Nizhnii Tagil
Kozlov et al. (2011)
South Africa
 
  • Limpopo
    • Waterberg District Municipality
      • Modimolle-Mookgophong Local Municipality
        • Mookgophong
McDonald et al. (1995) +1 other reference
 
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