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Davreuxite

A valid IMA mineral species - grandfathered
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About DavreuxiteHide

Formula:
MnAl6Si4O17(OH)2
Colour:
Creamy-white, pale rose pink
Hardness:
2 - 3
Specific Gravity:
3.30 - 3.38
Crystal System:
Monoclinic
Name:
Originally reported and described by de Koninck in 1878. Named after Belgian pharmacist, natural scientist, and Professor of Mineralogy at the University of Liège Charles Joseph Davreux (Liège, Belgium 10th September 1800 - Liège, Belgium 11th April 1863).
This page provides mineralogical data about Davreuxite.


Unique IdentifiersHide

Mindat ID:
1237
Long-form identifier:
mindat:1:1:1237:5

IMA Classification of DavreuxiteHide

Classification of DavreuxiteHide

9.BF.15

9 : SILICATES (Germanates)
B : Sorosilicates
F : Sorosilicates with mixed SiO4 and Si2O7 groups; cations in tetrahedral [4] and greater coordination
58.1.2.1

58 : SOROSILICATES Insular, Mixed, Single, and Larger Tetrahedral Groups
1 : Insular, Mixed, Single, and Larger Tetrahedral Groups with cations in [4] and higher coordination; single and double groups (n=1, 2)
16.16.3

16 : Silicates Containing Aluminum and other Metals
16 : Aluminosilicates of Mn

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

Physical Properties of DavreuxiteHide

Transparency:
Transparent, Translucent
Colour:
Creamy-white, pale rose pink
Hardness:
2 - 3 on Mohs scale
Tenacity:
Brittle
Cleavage:
Distinct/Good
Good on {100}.
Comment:
Cross fractures on {010}.
Density:
3.30 - 3.38 g/cm3 (Measured)    3.34 g/cm3 (Calculated)

Optical Data of DavreuxiteHide

Type:
Biaxial (-)
RI values:
nα = 1.66 nβ = 1.684 nγ = 1.69
2V:
Measured: 48° , Calculated: 52°
Max. Birefringence:
δ = 0.030
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:
weak

Chemistry of DavreuxiteHide

Mindat Formula:
MnAl6Si4O17(OH)2
Element Weights:
Element% weight
O47.859 %
Al25.487 %
Si17.687 %
Mn8.649 %
H0.317 %

Calculated from ideal end-member formula.
O
Al
Si
Mn
H
Common Impurities:
Ti,Fe,Cr,Cu,Zn,Mg,P

Crystallography of DavreuxiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Setting:
P21/m
Cell Parameters:
a = 9.55 Å, b = 5.77 Å, c = 12.88 Å
β = 116.82°
Ratio:
a:b:c = 1.655 : 1 : 2.232
Unit Cell V:
633.39 ų (Calculated from Unit Cell)
Z:
2

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000955DavreuxiteSahl K, Jones P G, Sheldrick G M (1984) The crystal structure of davreuxite, MnAl6Si4O17(OH)2 American Mineralogist 69 783-78719840293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.511 Å(100)
2.870 Å(60)
3.103 Å(45)
4.290 Å(40)
5.719 Å(35)
2.840 Å(35)
8.51 Å(30)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 5: Initiation of plate tectonics<3.5-2.5
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Type Occurrence of DavreuxiteHide

General Appearance of Type Material:
fibrous masses in quartz veins, in close association with pyrophyllite and kaolinite.
Place of Conservation of Type Material:
Royal Belgium Institute of Natural Sciences, Brussels
Mineralogical Museum University of Wroclaw, Poland
Associated Minerals at Type Locality:

Other Language Names for DavreuxiteHide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Davreuxite associated with QuartzSiO2
1 photo of Davreuxite associated with Chlorite Group

Related Minerals - Strunz-mindat GroupingHide

9.BF.05HarstigiteCa6(Mn,Mg)Be4Si6(O,OH)24Orth. mmm(2/m2/m2/m)
9.BF.10SamfowleriteCa28Mn6Zn4(Be,Zn)4Be12[(OH)3(SiO4)3(Si2O7)2]4Mon. 2/m : P21/b
9.BF.20QueititePb4Zn2(SO4)(SiO4)(Si2O7)Mon. 2 : P21

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 DavreuxiteHide

References for DavreuxiteHide

Localities for DavreuxiteHide

Showing 9 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.
Belgium
 
  • Wallonia
    • Liège
      • Sankt-Vith
Fransolet et al. (1984) +1 other reference
    • Luxembourg
Michel Blondieau. +2 other references
H.J. Wilke collection
de Koninck (1878) +7 other references
Corin (1929) +2 other references
        • Cahay
Hatert et al. (2002)
Hatert et al. (2002)
Blondieau (2005)
Germany
 
  • Saxony-Anhalt
    • Mansfeld-Südharz
      • Mansfeld
Färber (n.d.)
 
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