Polekhovskyite (original) (raw)

A valid IMA mineral species

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Specific Gravity:

6.626 (Calculated)

Name:

Named in honor of Yury Stepanovich Polekhovsky (Юрий Степанович Полеховский) (1947–2018), Russian geologist and mineralogist, for his contributions to the studies of opaque minerals, including phosphides.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:53415:0

503458e1-dbe0-4dc7-987b-cb50c2879ae3

IMA Classification of PolekhovskyiteHide

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Classification of PolekhovskyiteHide

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1.BD.45

1 : ELEMENTS (Metals and intermetallic alloys; metalloids and nonmetals; carbides, silicides, nitrides, phosphides)
B : Metallic Carbides, Silicides, Nitrides, Phosphides and Hydrides
D : Phosphides

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
Pkh 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 PolekhovskyiteHide

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Hardness Data:

Could not be measured

Comment:

Could not be measured due to the small crystal size.

Density:

6.626 g/cm3 (Calculated)

Comment:

Calculated value based on the empirical formula.

Chemistry of PolekhovskyiteHide

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Crystallography of PolekhovskyiteHide

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Class (H-M):

6/m m m _(_6/_m_2/_m_2/m ) - Dihexagonal Dipyramidal

Cell Parameters:

a = 3.330(1) Å, c = 11.227(4) Å

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
5.614 Å (4)
2.884 Å (71)
2.807 Å (14)
2.793 Å (9)
2.565 Å (8)
2.011 Å (100)
1.665 Å (35)
1.432 Å (9)

Geological EnvironmentHide

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Type Occurrence of PolekhovskyiteHide

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General Appearance of Type Material:

Micrometer-sized euhedral crystals (to 3 μm).

Place of Conservation of Type Material:

Collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 5287/1.

Empirical Formula of Type Material:

Mo0.99(Ni0.83Fe0.18)1.01P2.01

Chemical Analysis of Type Material:

Mo 44.10 %
Ni 22.73 %
Fe 4.60 %
P 29.02 %
Total: 100.45 %

Geological Setting of Type Material:

Pyrometamorphic rocks; altered diopside microbreccia.

Associated Minerals at Type Locality:

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Other InformationHide

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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 PolekhovskyiteHide

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Reference List:

Britvin, Sergey N., Murashko, Mikhail N., Vereshchagin, Oleg S., Vapnik, Yevgeny, Shilovskikh, Vladimir V., Vlasenko, Natalia S., Permyakov, Vitalii V. (2022) Expanding the speciation of terrestrial molybdenum: Discovery of polekhovskyite, MoNiP2, and insights into the sources of Mo-phosphides in the Dead Sea Transform area. American Mineralogist, 107 (12) 2201-2211 doi:10.2138/am-2022-8261

Localities for PolekhovskyiteHide

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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.

Locality ListHide

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- 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.

Israel (TL)
Southern District (HaDarom District) Tamar Regional Council Hatrurim Basin Halamish wadi (Ẕuq Tamrur) (TL) Miyawaki et al. (2019) +1 other reference
Jordan
Amman Governorate Transjordan Plateau Vereshchagin et al. (2024)