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Magbasite

A valid IMA mineral species
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About MagbasiteHide

Formula:
KBaFe3+Mg7Si8O22(OH)2F6
Originally assumed to be considerably Sc-bearing.
Colour:
Colorless to pinkish violet
Lustre:
Vitreous
Hardness:
5
Specific Gravity:
3.41
Crystal System:
Orthorhombic
Name:
Named by I.E. Semenov, A.R. Khomyakov, A.V. Bukova in 1965 for the chemical composition that includes the elements MAGnesium and BArium.
Structurally related to carpholite.


Unique IdentifiersHide

Mindat ID:
2531
Long-form identifier:
mindat:1:1:2531:3

Similar NamesHide

MegabasitA synonym of Hübnerite

IMA Classification of MagbasiteHide

Approved
First published:
1965

Classification of MagbasiteHide

9.HA.25

9 : SILICATES (Germanates)
H : Unclassified silicates
A : With Alkali and Alkali-earth Elements
69.2.1c.1

69 : INOSILICATES Chains with Side Branches or Loops
2 : Chains with Side Branches or Loops with P>2
17.2.10

17 : Silicates Containing other Anions
2 : Silicates with fluoride

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

Physical Properties of MagbasiteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Colorless to pinkish violet
Hardness:
Density:
3.41 g/cm3 (Measured)    3.374 g/cm3 (Calculated)

Optical Data of MagbasiteHide

Type:
Biaxial (-)
RI values:
nα = 1.597(1) nβ = 1.609(1) nγ = 1.615(1)
2V:
Measured: 70° , Calculated: 70°
Max. Birefringence:
δ = 0.018
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:
High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r < v weak
Optical Extinction:
X = a, Y = b, Z = c.
Pleochroism:
Visible
Comments:
Z = lavender, X = pale lavender, Y = colorless.
Comments:
Absorption: Z > X > Y.

Chemistry of MagbasiteHide

Mindat Formula:
KBaFe3+Mg7Si8O22(OH)2F6

Originally assumed to be considerably Sc-bearing.
Element Weights:
Element% weight
O34.069 %
Si19.935 %
Mg15.095 %
Ba12.184 %
F10.114 %
Fe4.955 %
K3.469 %
H0.179 %

Calculated from ideal end-member formula.
O
Si
Mg
Ba
F
Fe
K
H
Common Impurities:
Ca

Crystallography of MagbasiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Cmma
Cell Parameters:
a = 18.9506(3) Å, b = 22.5045(3) Å, c = 5.2780(1) Å
Ratio:
a:b:c = 0.842 : 1 : 0.235
Unit Cell V:
2250.93 ų
Z:
4
Morphology:
As bundles of prismatic and acicular crystals
Comment:
Space group Cmme (Cmma).

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020127MagbasiteWelch M D, Mitchell R H, Kampf A R, Chakhmouradian, Smith D, Carter M (2014) Crystal structure and topological affinities of magbasite, KBaFe3+Mg7Si8O22(OH)2F6: a trellis structure related to amphibole and carpholite Mineralogical Magazine 78 29-452014Eldor carbonatite complex, Labrador Trough, Quebec, Canada0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.572 Å(100)
2.991 Å(68)
3.546 Å(47)
2.416 Å(41)
2.848 Å(39)
2.306 Å(38)
1.6336 Å(38)
Comments:
Eldor carbonatite complex, Quebec, Canada. Data from Welch et al. (2014).

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
Stage 4b: Highly evolved igneous rocks>3.0
36 : Carbonatites, kimberlites, and related igneous rocks

Type Occurrence of MagbasiteHide

General Appearance of Type Material:
Fan-shaped fine acicular and felt-like deposits up to 5 mm in size, somewhat resembling tremolite.
Place of Conservation of Type Material:
Ferman Mineralogical Museum, Moscow, Russia, number 73225 (type).
Geological Setting of Type Material:
Associated with alkalic barkevitic granosyenites occurring in dolomites.
Associated Minerals at Type Locality:

Other Language Names for MagbasiteHide

Dutch:Magbasiet
German:Magbasit
Spanish:Magbasita

Related Minerals - Strunz-mindat GroupingHide

9.HA.ShinichengiteCa5[BSi2O7(OH)2]2 · 6H2OTric. 1 : P1
9.HA.Kalyuzhnyite-(Ce)NaKCaSrCeTi(Si8O21)OF(H2O)3Mon. 2/m : P2/b
9.HA.MoragiteCa3TiSi2(Al2Si)O14Trig. 32 : P321
9.HA.05ErtixiiteNa2Si4O9Iso.
9.HA.10KenyaiteNa2Si22O41(OH)8 · 6H2OMon.
9.HA.20WawayandaiteCa6Mn2BBe9Si6O23(OH,Cl)15Mon.
9.HA.35DemagistrisiteBaCa2Mn3+4(Si3O10)(Si2O7)(OH)4 · 3H2OOrth. mm2 : Amm2
9.HA.37DonwilhelmsiteCaAl4Si2O11Hex. 6/mmm(6/m2/m2/m) : P63/mmc
9.HA.40KasatkiniteBa2Ca8B5Si8O32(OH)3 · 6H2O Mon.
9.HA.40'Igumnovite'Ca3Al2[SiO4]2[◻Cl4]Iso.
9.HA.42PaqueiteCa3TiSi2(Al,Ti,Si)3O14Trig. 32 : P321
9.HA.42QeltiteCa3TiSi2(Fe3+2Si)O14Trig. 32 : P321
9.HA.45RippiteK2(Nb,Ti)2(Si4O12)O(O,F)Tet.
9.HA.47ZagamiiteCaAl2Si3.5O11Hex. 6/mmm(6/m2/m2/m) : P63/mmc
9.HA.50RudenkoiteSr3(Al3.5Si3.5)O10(OH,O)8Cl2 · H2OMon.
9.HA.50'α-Carnegieite'NaAlSiO4
9.HA.52'Atheriastite'near Ca5MgFeAl6Si8O32 · 5H2O
9.HA.55'Foshallasite'Ca3[Si2O7] · 3H2O(?)
9.HA.57'Bhreckite'
9.HA.60NagelschmidtiteCa7(SiO4)2(PO4)2Hex. 6 : P61
9.HA.65Caryochroite[Na(Sr0.5Ca0.5)Mg]3[Fe3+8Mn(Fe2+0.5◻0.5)]10(Ti2Si12O37)(OH)14(H2O)3 Mon. 2/m
9.HA.70JuaniteCa10Mg4Al2Si11O39 · 4H2O or nearOrth.
9.HA.75TacharaniteCa12Al2Si18O33(OH)36Mon.
9.HA.80OyeliteCa10Si8B2O29 · 12.5H2OTric. 1 : P1
9.HA.85DenisoviteK14+x(Ca,Na,Mn,Fe)48[Si60O162]F16(Ox,OH4-x) · 2H2OMon.
9.HA.90TiettaiteK4Na12Fe3+Si16O41(OH)4 · 2H2OOrth. mmm(2/m2/m2/m) : Cmcm

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 3.4690% 1,075 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity: –

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

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 MagbasiteHide

References for MagbasiteHide

Localities for MagbasiteHide

Showing 4 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.
Canada
 
  • Québec
    • Nord-du-Québec
      • Nunavik
Mitchell et al. (2017)
          • Ashram Zone
Mitchell et al. (2017)
China (TL)
 
  • Inner Mongolia
    • Baotou City
      • Bayan Obo mining district
Semenov et al. (1965) +1 other reference
Xue et al. (2026)
 
and/or  
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