Badakhshanite-(Y) (original) (raw)
A valid IMA mineral species
Formula:
Y2Mn4Al(Si2B7BeO24)
Specific Gravity:
4.41 (Calculated)
Crystal System:
Orthorhombic
Name:
Named for the Gorno-Badakhshan Oblast, Tajikistan, that includes the type locality. The oblast makes up 45% of the land area of the country but holds only 3% of its population.
Related to perettiite-(Y) of which it is the AlBe-analogue.
Crystal structure details:
- tetrahedra form layers || (010) comprising of four different tetrahedrally coordinated sites: Si, B(1), B(2), and T;
- the above elements constitute 4-, 5-, and 8-membered rings of the Si2B7BeO24 composition;
- 3 cation sites between the above sheets: M(1), occupied by Y(REE); M(2), occupied by Mn2+(Y,Ca,Fe2+); and M(3), occupied by Al(Sc);
- ideal composition of the M(1,2) sites is Y2Mn4;
- M(3) site is, ideally, 1 Al apfu
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:53212:5
26ddbead-3373-4ead-b7ca-8d14becb26b2
IMA Classification of Badakhshanite-(Y)Hide
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Type description reference:
Pautov, Leonid A., Mirakov, Mirak A., Cámara, Fernando, Sokolova, Elena, Hawthorne, Frank C., Schodibekov, Manuchekhr A., Karpenko, Vladimir Yu. (2020) Badakhshanite-(Y), Y2Mn4Al(Si2B7BeO24), a new mineral species of the perettiite group from a granite miarolic pegmatite in Eastern Pamir, the Gorno Badakhshan Autonomous Oblast, Tajikistan. The Canadian Mineralogist, 58 (3) 381-394 doi:10.3749/canmin.2000003
Classification of Badakhshanite-(Y)Hide
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9.EA.45
9 : SILICATES (Germanates)
E : Phyllosilicates
A : Single nets of tetrahedra with 4-, 5-, (6-), and 8-membered rings
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 |
---|---|---|
Bad-Y | 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 Badakhshanite-(Y)Hide
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Comment:
Transparent and pale yellow in thin section.
Density:
4.41 g/cm3 (Calculated)
Comment:
Density calculated using the empirical formula. It is 4.25 g/cm3 using the ideal formula.
Optical Data of Badakhshanite-(Y)Hide
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RI values:
_n_α = 1.805(2) _n_β = 1.827 _n_γ = 1.853(3)
δ = 0.048
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Optical Extinction:
Straight extinction, negative elongation.
Chemistry of Badakhshanite-(Y)Hide
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Mindat Formula:
Y2Mn4Al(Si2B7BeO24)
Crystallography of Badakhshanite-(Y)Hide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 12.852(1) Å, b = 4.5848(5) Å, c = 12.8539(8) Å
Ratio:
a:b:c = 2.803 : 1 : 2.804
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
9.07 Å | (45) |
4.59 Å | (42) |
4.07 Å | (39) |
3.042 Å | (100) |
2.637 Å | (68) |
2.533 Å | (60) |
2.119 Å | (32) |
1.828 Å | (36) |
Geological EnvironmentHide
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Type Occurrence of Badakhshanite-(Y)Hide
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General Appearance of Type Material:
Single, columnar crystals, 50 to 400 μm in length, as inclusions in spessartine and tourmaline; rarely: crystals within blebs along garnet-tourmaline-quartz boudaries.
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 5235/1.
Geological Setting of Type Material:
Medium- to coarse-grained, non-graphic, miarolitic granitic pegmatite.
Associated Minerals at Type Locality:
Reference:
Pautov, L.A., Mirakov, M.A., Cámara, F., Sokolova, E., Hawthorne, F.C., Schodibekov, M.A., Karpenko, V.Yu. (2020) Badakhshanite-(Y), Y2Mn4Al(Si2B7BeO24), a New Mineral Species of the Perettiite Group from a Granite Miarolic Pegmatite in Eastern Pamir, the Gorno Badakhshan Autonomous Oblast, Tajikistan. The Canadian Mineralogist: 58(3): 381–394.
Synonyms of Badakhshanite-(Y)Hide
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Related Minerals - Strunz-mindat GroupingHide
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9.EA. | Bussyite-(Y) | (Y,REE,Ca)3(Na,Ca)6MnSi9Be5(O,OH,F)34 | Mon. 2 : _B_2 |
---|---|---|---|
9.EA. | Fluorapophyllite-(NH₄) | NH4Ca4(Si8O20)F · 8H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m n c |
9.EA. | Hydroxymcglassonite-(K) | KSr4Si8O20(OH) · 8H2O | Tet. |
9.EA. | Miyawakiite-(Y) | ◻Y4Fe2(Si8O20)(CO3)4(H2O)3 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_4/m c m |
9.EA.05 | Cuprorivaite | CaCuSi4O10 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n c c |
9.EA.05 | Gillespite | BaFe2+Si4O10 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n c c |
9.EA.05 | Effenbergerite | BaCuSi4O10 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n c c |
9.EA.05 | Wesselsite | SrCuSi4O10 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/n c c |
9.EA.07 | Fluorapophyllite-(Cs) | CsCa4(Si8O20)F · 8H2O | Tet. |
9.EA.10 | Ekanite | Ca2ThSi8O20 | Tet. 422 : _I_422 |
9.EA.15 | Fluorapophyllite-(K) | KCa4(Si8O20)(F,OH) · 8H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m n c |
9.EA.15 | Hydroxyapophyllite-(K) | KCa4(Si8O20)(OH,F) · 8H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) |
9.EA.15 | Fluorapophyllite-(Na) | NaCa4(Si8O20)F · 8H2O | Orth. |
9.EA.20 | Magadiite | Na2Si14O29 · 11H2O | Orth. m _m_2 : F d _d_2 |
9.EA.25 | Dalyite | K2ZrSi6O15 | Tric. 1 : _P_1 |
9.EA.25 | Davanite | K2TiSi6O15 | Tric. |
9.EA.30 | Sazhinite-(Ce) | Na2CeSi6O14 · 6H2O | Orth. m _m_2 : P m _m_2 |
9.EA.30 | Sazhinite-(La) | Na3La[Si6O15] · 2H2O | Orth. m _m_2 : P m _m_2 |
9.EA.35 | Armstrongite | CaZr[Si6O15] · 3H2O | Mon. 2/m : _B_2/m |
9.EA.40 | Okenite | Ca10Si18O46 · 18H2O | Tric. 1 : _P_1 |
9.EA.45 | Nekoite | Ca3Si6O15 · 7H2O | Tric. 1 : _P_1 |
9.EA.45 | Perettiite-(Y) | Y2Mn4FeSi2B8O24 | Orth. m m m _(_2/_m_2/_m_2/m ) : P m n a |
9.EA.47 | Shlykovite | KCa[Si4O9(OH)] · 3H2O | Mon. 2/m : _P_21/b |
9.EA.50 | Cavansite | Ca(VO)Si4O10 · 4H2O | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.EA.50 | Diegogattaite | Na2CaCu2Si8O20 · H2O | Mon. 2/m : _B_2/m |
9.EA.52 | Yangite | PbMnSi3O8 · H2O | Tric. 1 : _P_1 |
9.EA.55 | Pentagonite | Ca(VO)Si4O10 · 4H2O | Orth. m _m_2 |
9.EA.60 | Penkvilksite | Na4Ti2Si8O22 · 4H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c n |
9.EA.60 | Tumchaite | Na2Zr(Si4O11) · 2H2O | Mon. 2/m : _P_21/b |
9.EA.65 | Nabesite | Na2BeSi4O10 · 4H2O | Orth. 222 : _P_212121 |
9.EA.70 | Ajoite | (K,Na)Cu7AlSi9O24(OH)6 · 3H2O | Tric. |
9.EA.75 | Zeravshanite | Na2Cs4Zr3[Si18O45]*2H2O | Mon. 2/m : _B_2/b |
9.EA.80 | Bussyite-(Ce) | (Ce,REE)3(Na,H2O)6MnSi9Be5(O,OH)30F4 | Mon. 2/m : _B_2/b |
9.EA.85 | Plumbophyllite | Pb2Si4O10 · H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c n |
Fluorescence of Badakhshanite-(Y)Hide
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Other InformationHide
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IR Spectrum:
confirms lacking OH and H2O
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 Badakhshanite-(Y)Hide
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References for Badakhshanite-(Y)Hide
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Reference List:
Pautov, Leonid A., Mirakov, Mirak A., Cámara, Fernando, Sokolova, Elena, Hawthorne, Frank C., Schodibekov, Manuchekhr A., Karpenko, Vladimir Yu. (2020) Badakhshanite-(Y), Y2Mn4Al(Si2B7BeO24), a new mineral species of the perettiite group from a granite miarolic pegmatite in Eastern Pamir, the Gorno Badakhshan Autonomous Oblast, Tajikistan. The Canadian Mineralogist, 58 (3) 381-394 doi:10.3749/canmin.2000003
Localities for Badakhshanite-(Y)Hide
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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.
Tajikistan (TL) | |
---|---|
Gorno-Badakhshan Murghob ⓘ Dorozhnyi pegmatite (TL) | Pautov et al. (2020) |