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Axinite-(Mg)

A valid IMA mineral species
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About Axinite-(Mg)Hide

Formula:
Ca2MgAl2BSi4O15OH
Colour:
Colourless, pale blue, lavender, pink, brown
Lustre:
Vitreous
Hardness:
6½ - 7
Specific Gravity:
3.16
Crystal System:
Triclinic
Member of:
Name:
From the Greek αξίνα ("axina") for "axe", in allusion to the common habit of its crystals, and magnesium dominance in the formula.
Axinite Group. The magnesium analogue of Axinite-(Fe) and Axinite-(Mn).




Unique IdentifiersHide

Mindat ID:
2490
Long-form identifier:
mindat:1:1:2490:3

Similar NamesHide

AxinitA synonym of 'Axinite'
AxiniteA synonym of Axinite Group
Axinite-(Fe)A valid IMA mineral species - grandfatheredCa2Fe2+Al2BSi4O15OH
Axinite-(Fe)-Axinite-(Mn) SeriesA solid-solution series between two end-member minerals
Axinite-(Mn)A valid IMA mineral species - grandfatheredCa2Mn2+Al2BSi4O15(OH)
Axinite-(Mn)-Tinzenite SeriesA solid-solution series between two end-member minerals

IMA Classification of Axinite-(Mg)Hide

Approved
IMA Formula:
Ca4Mg2Al4[B2Si8O30](OH)2
Approval year:
1975

Classification of Axinite-(Mg)Hide

9.BD.20

9 : SILICATES (Germanates)
B : Sorosilicates
D : Si2O7 groups, with additional anions; cations in tetrahedral [4] and greater coordination
56.2.2.2

56 : SOROSILICATES Si2O7 Groups, With Additional O, OH, F and H2O
2 : Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordination
17.5.29

17 : Silicates Containing other Anions
5 : Borosilicates

Mineral SymbolsHide

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

Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.

SymbolSourceReference for Standard
Ax-MgIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43
AxKretz (1983)Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279.
AxSiivolam & Schmid (2007)Siivolam, J. and Schmid, R. (2007) Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: List of mineral abbreviations. Web-version 01.02.07. IUGS Commission on the Systematics in Petrology. download
AxWhitney & Evans (2010)Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371

Pronunciation of Axinite-(Mg)Hide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of Axinite-(Mg)Hide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Colourless, pale blue, lavender, pink, brown
Streak:
White
Hardness:
6½ - 7 on Mohs scale
Density:
3.16(1) g/cm3 (Measured)    3.167 g/cm3 (Calculated)

Optical Data of Axinite-(Mg)Hide

Type:
Biaxial (-)
RI values:
nα = 1.672 - 1.693 nβ = 1.677 - 1.701 nγ = 1.681 - 1.704
2V:
Measured: 69° to 87°, Calculated: 62° to 82°
Max. Birefringence:
δ = 0.009 - 0.011
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:
Very 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:
strong

Chemistry of Axinite-(Mg)Hide

Mindat Formula:
Ca2MgAl2BSi4O15OH
Element Weights:
Element% weight
O47.531 %
Si20.859 %
Ca14.883 %
Al10.020 %
Mg4.513 %
B2.007 %
H0.187 %

Calculated from ideal end-member formula.
O
Si
Ca
Al
Mg
B
H
Common Impurities:
Ti,V,Mn,Zn,K,H2O

Crystallography of Axinite-(Mg)Hide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 7.1381(3) Å, b = 9.1626(4) Å, c = 8.9421(4) Å
α = 91.903(4)°, β = 98.105(3)°, γ = 77.468(4)°
Ratio:
a:b:c = 0.779 : 1 : 0.976
Unit Cell V:
565.21 ų (Calculated from Unit Cell)
Z:
2

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006850Axinite-(Mg)Andreozzi G B, Lucchesi S, Graziani G (2000) Structural study of magnesioaxinite and its crystal-chemical relations with axinite-group minerals European Journal of Mineralogy 12 1185-119420000293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.95 Å(15)
6.29 Å(25)
4.96 Å(4)
4.76 Å(8)
4.61 Å(2)
3.97 Å(10)
3.66 Å(5)
3.44 Å(65)
3.27 Å(20)
3.14 Å(65)
3.07 Å(8)
2.985 Å(20b)
2.877 Å(20)
2.796 Å(100)
2.753 Å(5b)
2.633 Å(5)
2.556 Å(25)
2.429 Å(18)
2.415 Å(18)
2.452 Å(8)
2.305 Å(1)
2.252 Å(1)
2.176 Å(30)
2.150 Å(30)
2.121 Å(4)
2.048 Å(14)
2.028 Å(14)
Comments:
ICDD 29-344, natural material, Tanzania

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of Axinite-(Mg)Hide

Synonyms of Axinite-(Mg)Hide

Other Language Names for Axinite-(Mg)Hide

Relationship of Axinite-(Mg) to other SpeciesHide

Member of:
Other Members of Axinite Group:
Axinite-(Fe)Ca2Fe2+Al2BSi4O15OHTric. 1 : P1
Axinite-(Mn)Ca2Mn2+Al2BSi4O15(OH)Tric. 1 : P1
TinzeniteCa2Mn2+4Al4[B2Si8O30](OH)2Tric. 1 : P1

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Axinite-(Mg) associated with GraphiteC

Related Minerals - Strunz-mindat GroupingHide

9.BD.05BertranditeBe4(Si2O7)(OH)2Orth. mm2 : Cmc21
9.BD.10HemimorphiteZn4Si2O7(OH)2 · H2OOrth. mm2 : Imm2
9.BD.15JunitoiteCaZn2Si2O7 · H2OOrth. mm2 : Aba2
9.BD.20TinzeniteCa2Mn2+4Al4[B2Si8O30](OH)2Tric. 1 : P1
9.BD.20Axinite-(Fe)Ca2Fe2+Al2BSi4O15OHTric. 1 : P1
9.BD.20DubińskaiteCa4Sc2Al4[Be2Si8O30](OH)2Tric. 1 : P1
9.BD.20Axinite-(Mn)Ca2Mn2+Al2BSi4O15(OH)Tric. 1 : P1
9.BD.25VistepiteSnMn4B2Si4O16(OH)2Tric. 1 : P1
9.BD.30BoralsiliteAl16B6O30(Si2O7)Mon. 2/m : B2/m
9.BD.35Werdingite(Mg,Fe)2Al14Si4B4O37Tric. 1 : P1
9.BD.40VránaiteAl16B4Si4O38Mon. 2/m : B2/m

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 Axinite-(Mg)Hide

References for Axinite-(Mg)Hide

Localities for Axinite-(Mg)Hide

Showing 20 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.
Australia
 
  • New South Wales
    • Murray Co.
      • Queanbeyan
        • Googong Dam
Leavens et al. (1980) +1 other reference
  • Tasmania
    • West Coast municipality
      • Zeehan mining district
R. Bottrill
Austria
 
  • Lower Austria
    • Krems-Land District
      • Spitz
Niedermayr (2002)
  • Salzburg
    • Zell am See District
      • Bramberg am Wildkogel
Niedermayr (1996)
Czech Republic
 
  • South Moravian Region
    • Blansko District
Novák et al. (2002)
  • Vysočina Region
    • Havlíčkův Brod District
      • Golčův Jeníkov
Dolníček Z et al. (2020)
Japan
 
  • Nagano Prefecture
    • Kashio
Matsubara et al. (2011)
Namibia
 
  • Erongo Region
    • Dâures Constituency
Grolig (2005) +1 other reference
Romania
 
  • Maramureș County
    • Târgu Lăpuș
HÎRTOPANU et al. (2025)
Russia
 
  • Chelyabinsk Oblast
    • Satkinsky District
Erokhin et al. (2007)
Spain
 
  • Andalusia
    • Córdoba
      • Adamuz
Calvo Rebollar (2018)
Sweden
 
  • Värmland County
    • Filipstad
Gatedal (2003)
Switzerland
 
  • Valais
    • Goms
      • Obergoms
        • Oberwald
          • Gere (Geren)
Tanzania
 
Mineralogical Society of America - ...
  • Manyara Region
    • Simanjiro District
      • Lelatema Mountains
P Bongaerts collection +2 other references
Photo ID: 379162
USA
 
  • California
    • Butte County
Chris Stefano
  • Michigan
    • Marquette County
      • Marquette
Heinrich et al. (2004)
  • Nevada
    • Mineral County
      • Fitting Mining District
Rocks & Minerals. Nov. 1999.
        • Luning
Leavens et al. (1980)
 
and/or  
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