Komkovite (original) (raw)

A valid IMA mineral species

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About KomkoviteHide

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Formula:

BaZr[Si3O9] · 3H2O

Name:

Named in honor of Aleksandr Ivanovich Komkov (Александр Иванович Комков) (1926-1987), mineralogist and crystallographer at the Karpinskii All-Union Research Institute of Geology, St. Petersburg, Russia.

Possibly formed (type material) by alteration of catapleiite.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:2247:3

d8cc8152-f58c-4c7c-b7ce-34a821c166e8

IMA Classification of KomkoviteHide

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IMA Formula:

BaZrSi3O9 · 3H2O

Type description reference:

Classification of KomkoviteHide

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9.DM.10

9 : SILICATES (Germanates)
D : Inosilicates
M : Inosilicates with 6-periodic single chains

59.2.4.1

59 : CYCLOSILICATES Three-Membered Rings
2 : Three-Membered Rings, hydrated

14.10.31

14 : Silicates not Containing Aluminum
10 : Silicates of Zr or Hf

Mineral SymbolsHide

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

Symbol Source Reference
Kkv 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 KomkoviteHide

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Density:

3.31 g/cm3 (Measured) 3.31 g/cm3 (Calculated)

Optical Data of KomkoviteHide

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RI values:

_n_ω = 1.671 _n_ε = 1.644

δ = 0.027

Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.

Chemistry of KomkoviteHide

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Mindat Formula:

BaZr[Si3O9] · 3H2O

Common Impurities:

Hf,Fe,Ca,K

Crystallography of KomkoviteHide

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Class (H-M):

32 - Trapezohedral

Cell Parameters:

a = 10.52 Å, c = 15.73 Å

Unit Cell V:

1,507.62 ų (Calculated from Unit Cell)

Crystal StructureHide

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ID Species Reference Link Year Locality Pressure (GPa) Temp (K)
0012485 Komkovite Sokolova E V, Araktscheeva A V, Voloshin A V (1991) Crystal structure of komkovite Doklady Akademii Nauk SSSR 320 1384-1388 1991 0 293
0015621 Komkovite Sokolova E V, Arakcheeva A V, Voloshin A V (1991) Crystal structure of komkovite Soviet Physics Doklady 36 666-668 1991 0 293

CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
5.23 Å (100)
2.96 Å (90)
3.59 Å (80)
3.02 Å (80)
2.57 Å (60)
2.106 Å (60)

Geological EnvironmentHide

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Type Occurrence of KomkoviteHide

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General Appearance of Type Material:

Equant crystals, 1-5 mm across, with trigonal pyramidal faces.

Place of Conservation of Type Material:

Geology Museum, Kola Branch, Academy of Sciences, Apatity.
Mining Institute, St. Petersburg, 2037/1.
A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, p462/1.

Geological Setting of Type Material:

In dolomitic veinlets that cut metasomatically altered pyroxenites in a carbonatite complex.

Associated Minerals at Type Locality:

Reference:

Voloshin, A.V., Pakhomovskiy, Y.Y., Men'shikov, Y.P., Sokolova, Y.V., Yegorov-Tismenko, Y.K. (1990) Komkovite - A new hydrous barium zirconosilicate from the carbonatites of Vuoriyarvi (Kola Peninsula). Mineralogiceskij Zhurnal: 12: 69-73.

Synonyms of KomkoviteHide

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Other Language Names for KomkoviteHide

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Relationship of Komkovite to other SpeciesHide

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Other Members of this group:

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Fluorescence of KomkoviteHide

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Other InformationHide

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IR Spectrum:

Absorption features at 3540, 3510, 1665, 1650, 1045, 970, 920, 740, 545, and 495 cm-1. The first four correspond to molecular H2O.

Thermal Behaviour:

One endothermic peak at 140 °C corresponding to the maximum loss of H2O, which is lost completely at 600 °C.

Notes:

Light blue cathodoluminescence.

Health Risks:

No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

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References for KomkoviteHide

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Localities for KomkoviteHide

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ⓘ - 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 Northern Karelia Vuoriyarvi alkaline-ultrabasic massif (TL) Voloshin et al. (1990) +2 other references