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Podlesnoite

A valid IMA mineral species
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About PodlesnoiteHide

01407420017271949433328.jpg
Aleksandr Semenovich Podlesnyi (podlesnoite)
Formula:
BaCa2(CO3)2F2
Colour:
Colorless, white
Lustre:
Vitreous
Hardness:
3½ - 4
Specific Gravity:
3.62
Crystal System:
Orthorhombic
Name:
Named in honor of Aleksandr Semenovich Podlesnyi (Александр Семенович Подлесный) (28 November 1948, Zabolottsi, Ivanichesky district, Volyn region, Ukraine, USSR – 13 October 2010), Russian amateur mineralogist and collector in recognition of his significant contributions to the mineralogy of the Khibiny massif. He worked in the Kirovskii underground mine, assembling the best systematic collection of Kirovskii mine minerals. He collected and provided for study the specimens which became the holotype specimens of eleven new species and the cotype specimens of four additional new species. Pronounced "pod-lez'-no-ite".
This page provides mineralogical data about Podlesnoite.


Unique IdentifiersHide

Mindat ID:
30907
Long-form identifier:
mindat:1:1:30907:7

IMA Classification of PodlesnoiteHide

Classification of PodlesnoiteHide

5.BC.15

5 : CARBONATES (NITRATES)
B : Carbonates with additional anions, without H2O
C : With alkali-earth cations
16a.2.5.1

16a : ANHYDROUS CARBONATES CONTAINING HYDROXYL OR HALOGEN
2 : (AB)3(XO3)2Zq

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

Physical Properties of PodlesnoiteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Colorless, white
Streak:
White
Hardness:
3½ - 4 on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
3.62(1) g/cm3 (Measured)    3.60 g/cm3 (Calculated)

Optical Data of PodlesnoiteHide

Type:
Biaxial (-)
RI values:
nα = 1.500 nβ = 1.612(2) nγ = 01.614(2)
2V:
Measured: 10° (5), Calculated: 14°
Max. Birefringence:
δ = 0.114
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:
Moderate
Pleochroism:
Non-pleochroic

Chemistry of PodlesnoiteHide

Mindat Formula:
BaCa2(CO3)2F2
Element Weights:
Element% weight
Ba36.572 %
O25.565 %
Ca21.347 %
F10.119 %
C6.397 %

Calculated from ideal end-member formula.

Crystallography of PodlesnoiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Cmcm
Cell Parameters:
a = 12.501(8) Å, b = 5.846(3) Å, c = 9.443(5) Å
Ratio:
a:b:c = 2.138 : 1 : 1.615
Unit Cell V:
690.1 ų
Z:
4
Morphology:
Prismatic crystals, radial spherulites.

Forms include {100}, {110}, {210}, {001}, {101}, {112}, {313}, {111} and {021}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011129PodlesnoiteZubkova N V, Pushcharovsky D Y, Pekov I V, Rabadanov M K (2007) The crystal structure of podlesnoite, BaCa2(CO3)2F2 Zeitschrift fur Kristallographie 222 474-4762007Kirovskii mine, Khibiny alkaline massif, Kola Peninsula, Russia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks

Type Occurrence of PodlesnoiteHide

General Appearance of Type Material:
Perfect prismatic crystals up to 1x1x4 mm typically combined in groups, and radial fibrous spherulites up to 8 mm in diameter.
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Moscow, Russia.
Geological Setting of Type Material:
In cavities within a hydrothermal lens-shaped body located in urtite rock.
Associated Minerals at Type Locality:

Synonyms of PodlesnoiteHide

Other Language Names for PodlesnoiteHide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Podlesnoite associated with NatroliteNa2Al2Si3O10 · 2H2O

Related Minerals - Strunz-mindat GroupingHide

5.BC.05BrenkiteCa2(CO3)F2Orth. mmm(2/m2/m2/m) : Pbcn
5.BC.10RouvilleiteNa3CaMn2+(CO3)3FMon. 2/m : B2/b

Fluorescence of PodlesnoiteHide

Prismatic crystals - pinkish orange in SW
Radial spherulites - bluish lilac SW, lilac-blue LW

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 PodlesnoiteHide

References for PodlesnoiteHide

Localities for PodlesnoiteHide

Showing 1 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.
Russia (TL)
 
  • Murmansk Oblast
    • Kukisvumchorr Mt
Pekov et al. (2008)
 
and/or  
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