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Krasnovite

A valid IMA mineral species
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About KrasnoviteHide

Formula:
Ba(Al,Mg)(PO4,CO3)(OH)2 · H2O
Colour:
Pale blue
Lustre:
Silky
Hardness:
2
Specific Gravity:
3.70
Crystal System:
Orthorhombic
Name:
Named in honor of Natalia Ivanovna Krasnova (Наталия Ивановна Краснова) (1941-), mineralogist at St. Petersburg University.
This page provides mineralogical data about Krasnovite.


Unique IdentifiersHide

Mindat ID:
7145
Long-form identifier:
mindat:1:1:7145:7

Similar NamesHide

KravtsoviteA valid IMA mineral speciesPdAg2S
KrásnoiteA valid IMA mineral speciesCa3Al7.7Si3P4O23.5(OH)12.1F2 · 8H2O

IMA Classification of KrasnoviteHide

Classification of KrasnoviteHide

8.DK.35

8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
K : With large and medium-sized cations, (OH, etc.):RO4 > 1:1 and < 2:1

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

Pronunciation of KrasnoviteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of KrasnoviteHide

Silky
Transparency:
Translucent
Colour:
Pale blue
Streak:
White
Hardness:
Cleavage:
Perfect
Two parallel to [010]
Density:
3.70(5) g/cm3 (Measured)    3.691 g/cm3 (Calculated)

Optical Data of KrasnoviteHide

Type:
Biaxial (-)
RI values:
nα = 1.616(2) nβ = 1.629(2) nγ = 1.64(2)
2V:
Measured: 70° to 90°, Calculated: 84°
Max. Birefringence:
δ = 0.024
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:
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 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.
Dispersion:
strong
Pleochroism:
Non-pleochroic

Chemistry of KrasnoviteHide

Mindat Formula:
Ba(Al,Mg)(PO4,CO3)(OH)2 · H2O
Element Weights:
Element% weight
Ba44.113 %
O35.976 %
P9.950 %
Al8.667 %
H1.295 %

Calculated from ideal end-member formula.
Ba
O
P
Al
H

Crystallography of KrasnoviteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 8.939(2) Å, b = 5.669(3) Å, c = 11.073(3) Å
Ratio:
a:b:c = 1.577 : 1 : 1.953
Unit Cell V:
561.13 ų (Calculated from Unit Cell)
Z:
4
Comment:
space group Pnna or Pnnn

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.768 Å(100)
3.479 Å(82)
5.54 Å(79)
2.543 Å(61)
3.345 Å(59)
2.072 Å(41)
2.354 Å(32)

Geological EnvironmentHide

Type Occurrence of KrasnoviteHide

General Appearance of Type Material:
Spherulites, up to 3 mm across, consisting of pale blue fibers.
Place of Conservation of Type Material:
Mineralogy Department of Saint Petersburg University and the Saint Petersburg Mining Institute, Russia.
Geological Setting of Type Material:
Dolomite carbonatite.
Associated Minerals at Type Locality:

Synonyms of KrasnoviteHide

Other Language Names for KrasnoviteHide

German:Krasnovit
Spanish:Krasnovita

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Krasnovite associated with AnalcimeNa(AlSi2O6) · H2O
1 photo of Krasnovite associated with AnkeriteCa(Fe2+,Mg)(CO3)2
1 photo of Krasnovite associated with SodaliteNa4(Si3Al3)O12Cl
1 photo of Krasnovite associated with DawsoniteNaAlCO3(OH)2

Related Minerals - Strunz-mindat GroupingHide

8.DK.RegeriteKFe6(PO4)4(OH)7(H2O)6 · 4H2OMon. 2/m : P21/b
8.DK.RichelsdorfiteCa2Cu5Sb(AsO4)4(OH)6Cl · 6H2OMon. 2/m : B2/m
8.DK.BimbowrieiteNaMgFe3+5(PO4)4(OH)6 · 2H2OMon. 2/m : B2/b
8.DK.PuttapaitePb2Mn2+2ZnCr3+4O2(AsO4)4(OH)6 · 12H2OMon. 2/m : B2/m
8.DK.10ThalliumpharmacosideriteTlFe3+4[(AsO4)3(OH)4] · 4H2OIso. 43m : F43m
8.DK.10NatropharmacosideriteNaFe3+4(AsO4)3(OH)4 · 4H2OIso. 43m : P43m
8.DK.10PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2OIso. 43m : P43m
8.DK.10PlumbopharmacosideritePb0.5Fe3+4(AsO4)3(OH)4 · 5H2OIso. 43m : P43m
8.DK.10StrontiopharmacosideriteSr0.5Fe3+4[(AsO4)3(OH)4] · 4H2OTet. 42m : P42m
8.DK.10BariopharmacosideriteBa0.5Fe3+4(AsO4)3(OH)4 · 5H2OTet. 42m : P42m
8.DK.10Hydroniumpharmacosiderite(H3O)Fe3+4(AsO4)3(OH)4 · 4H2OIso. 43m : P43m
8.DK.12Hydroniumpharmacoalumite(H3O)Al4(AsO4)3(OH)4 · 4.5H2OIso. 43m : P43m
8.DK.12BariopharmacoalumiteBa0.5Al4(AsO4)3(OH)4 · 4H2OIso. 43m : P43m
8.DK.12PharmacoalumiteKAl4(AsO4)3(OH)4 · 6.5H2OIso. 43m : P43m
8.DK.12CalciopharmacoalumiteCa0.5Al4(AsO4)3(OH)4 · 5H2OIso. 43m : P43m
8.DK.12NatropharmacoalumiteNaAl4(AsO4)3(OH)4 · 4H2OIso. 43m : P43m
8.DK.15MatioliiteNaMgAl5(PO4)4(OH)6 · 2H2OMon. 2/m : B2/b
8.DK.15BurangaiteNaFe2+Al5(PO4)4(OH)6 · 2H2OMon. 2/m : B2/b
8.DK.15NatrodufréniteNaFe3+Fe3+5(PO4)4O(OH)5(H2O)2Mon. 2/m : B2/b
8.DK.15DufréniteCa0.5Fe2+Fe3+5(PO4)4(OH)6 · 2H2OMon. 2/m : B2/b
8.DK.15GayiteNaMn2+Fe3+5(PO4)4(OH)6 · 2H2OMon. 2/m : B2/b
8.DK.20KidwelliteNaFe3+9+x(PO4)6(OH)11 · 3H2O, x = 0.33Mon. 2/m : P2/b
8.DK.25Bleasdaleite(Ca,Fe3+)2Cu5(Bi,Cu)(PO4)4(H2O,OH,Cl)13Mon. 2/m : B2/m
8.DK.30Matulaite(Fe3+,Al)Al7(PO4)4(PO3OH)2(OH)8(H2O)8 · 8H2OMon. 2/m

Other InformationHide

Notes:
Decomposes with effervescence in warm 10% HCl.
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 KrasnoviteHide

References for KrasnoviteHide

Localities for KrasnoviteHide

Showing 2 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.
Bolivia
 
  • Cochabamba
    • Ayopaya Province
Alfredo Petrov and Matthias Rheinlander ...
Russia (TL)
 
  • Murmansk Oblast
    • Kovdorsky District
      • Kovdor Massif
Britvin et al. (1996) +2 other references
 
and/or  
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