Faizievite (original) (raw)
A valid IMA mineral species
About FaizieviteHide
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Formula:
K2Na(Ca6Na)Ti4Li6[Si6O18]2[Si12O30]F2
Name:
Named in honor of Faiziev Abdulkhak Radzhabovitch (born 1938) of Dushanbe, Tadjikistan, professor and member-correspondent of the Academy of Sciences of the Republic of Tadjikistan.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:31306:1
d19c1008-e5e8-44c1-a3da-74944e1f820e
IMA Classification of FaizieviteHide
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IMA Formula:
Li6K2Na(Ca6Na)Ti4(Si6O18)2(Si12O30)F2
Type description reference:
Agakhanov, Atali A., Pautov, Leonid A., Uvarova, Yulia A., Sokolova, Elena V., Hawthorne, Frank C., Karpenko, Vladimir Y., Gafurov, Farhod G. (2007) Faizievite K2Na(Ca6Na)Ti4Li6Si24O66F2 – a New Mineral Species. New Data on Minerals, 42. Moscow. 5-10
Classification of FaizieviteHide
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9.CM.10
9 : SILICATES (Germanates)
C : Cyclosilicates
M : [Si6O18]12- 6-membered double rings (sechser-Doppelringe)
63.2.10.1
63 : CYCLOSILICATES Condensed Rings
2 : Condensed Rings (Milarite - Osumilite group)
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 |
---|---|---|
Fai | 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 FaizieviteHide
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Hardness:
VHN50=445 kg/mm2 - Vickers
Density:
2.83(2) g/cm3 (Measured) 2.819 g/cm3 (Calculated)
Optical Data of FaizieviteHide
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RI values:
_n_α = 1.651(2) _n_β = 1.655(2) _n_γ = 1.657(2)
2V:
Measured: 72° (2), Calculated: 70.4°
δ = 0.006
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of FaizieviteHide
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Mindat Formula:
K2Na(Ca6Na)Ti4Li6[Si6O18]2[Si12O30]F2
Crystallography of FaizieviteHide
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Class (H-M):
1 - Pinacoidal
Cell Parameters:
a = 9.8156(9) Å, b = 9.8249(9) Å, c = 17.3087(16) Å
α = 99.209(2)°, β = 94.67(2)°, γ = 119.839(1)°
Ratio:
a:b:c = 0.999 : 1 : 1.762
Unit Cell V:
1,403.74 ų (Calculated from Unit Cell)
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0006162 | Faizievite | Uvarova Yu A, Sokolova E, Hawthorne F C, Agakhanov A A, Pautov L A (2008) The crystal chemistry of faizievite, K2Li6Na(Ca6Na)Ti4[Si6O18]2[Si12O30]F2, a novel structure based on intercalated blocks of the baratovite and berezanskite structures The Canadian Mineralogist 46 163-171 | 2008 | Dara-i-Poiz glacier, Alai mountain ridge, Tien-Shan Mountains, Tajikistan | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.35 Å | (100) |
3.06 Å | (90) |
4.25 Å | (60) |
2.885 Å | (55) |
3.14 Å | (20) |
1.868 Å | (17) |
2.870 Å | (10) |
5.60 Å | (9) |
Comments:
Dara-i-Pioz glacier, Tajikistan. Data from the type description.
Geological EnvironmentHide
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Type Occurrence of FaizieviteHide
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General Appearance of Type Material:
Tabular plates without vicinal forms, and up to 0.3 cm in maximum dimension.
Place of Conservation of Type Material:
Fersman Mineralоgical Museum, Russian Academy of Science.
Geological Setting of Type Material:
Associated Minerals at Type Locality:
Reference:
Agakhanov, A.A., Pautov, L.A., Uvarova, Y.A., Sokolova, E.V., Hawthorne, F.C., Karpenko, V.Y., Gafurov, F.G. (2007) Faizievite, K2Na(Ca6Na)Ti4Li6Si24O66F2 - a new mineral species. New Data on Minerals. Moscow: 42: 5-10.
Synonyms of FaizieviteHide
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Other Language Names for FaizieviteHide
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Relationship of Faizievite to other SpeciesHide
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Structurally related to group(s):
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.CM. | Agakhanovite-(Y) | K◻2(YCa)Be3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
---|---|---|---|
9.CM.05 | Armenite | Ba(H2O)2Ca2Al3[Al3Si9O30] | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n a |
9.CM.05 | Brannockite | K◻2Sn2Li3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Chayesite | K◻2Mg2(Mg2Fe3+)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Darapiosite | KNa2Mn2(Zn2Li)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Eifelite | KNa2(MgNa)Mg3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Merrihueite | K(◻Na)Fe2+2Fe2+3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Milarite | K(◻H2O)Ca2(Be2Al)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Osumilite-(Mg) | K◻2Mg2Al3[Al2Si10O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Osumilite | K◻2Fe2+2Al3[Al2Si10O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Poudretteite | K◻2Na2B3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Roedderite | K(◻Na)Mg2Mg3[Si12O30] | Hex. 6_m_2 : P_62_c |
9.CM.05 | Sogdianite | K◻2Zr2Li3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Sugilite | KNa2Fe3+2Li3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Yagiite | Na◻2Mg2Al3[Al2Si10O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Berezanskite | K◻2Ti2Li3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Dusmatovite | K(K◻)Mn2+2Zn3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Shibkovite | K(◻K)Ca2Zn3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Almarudite | K◻2Mn2+2(Be2Al)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m m m |
9.CM.05 | Trattnerite | ◻(◻)2Fe3+2Mg3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Oftedalite | K◻2(ScCa)Be3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | Klöchite | K◻2(Fe2+Fe3+)Zn3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
9.CM.05 | Friedrichbeckeite | K(◻Na)Mg2(Be2Mg)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.05 | UM1990-73-SiO:KMnNaZn | K(KNa0.5◻0.5)(Mn1.5Na0.5)Zn3[Si12O30] | Hex. |
9.CM.05 | Laurentthomasite | K◻2Mg2(Be2Al)[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
9.CM.9.CM. | Aluminosugilite | KNa2Al2Li3[Si12O30] | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m c c |
Fluorescence of FaizieviteHide
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In shortwave ultraviolet light, it has a bright white luminescence; in longwave ultraviolet light, it does not luminesce.
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.
Internet Links for FaizieviteHide
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References for FaizieviteHide
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Reference List:
Agakhanov, Atali A., Pautov, Leonid A., Uvarova, Yulia A., Sokolova, Elena V., Hawthorne, Frank C., Karpenko, Vladimir Y., Gafurov, Farhod G. (2007) Faizievite K2Na(Ca6Na)Ti4Li6Si24O66F2 – a New Mineral Species. New Data on Minerals, 42. Moscow. 5-10
Uvarova, Y. A., Sokolova, E., Hawthorne, F. C., Agakhanov, A. A., Pautov, L. A. (2008) The crystal chemistry of faizievite, K2Li6Na(Ca6Na)Ti4[Si6O18]2[Si12O30]F2, a novel structure based on intercalated blocks of the baratovite and berezanskite structures. The Canadian Mineralogist, 46 (1) 163-171 doi:10.3749/canmin.46.1.163
Localities for FaizieviteHide
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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.