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Quintinite-2H

A structural variant of Quintinite
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About Quintinite-2HHide

Formula:
Mg4Al2(OH)12(CO3) · 3H2O
Colour:
Deep orange-red, orange, pale brown
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
2.14
Crystal System:
Hexagonal
Name:
Named in 1997 by George Y. Chao and Robert A. Gault in honor of Quintin Wight [b. April 23, 1935 Canada], of Ottawa, Ontario, Canada, significant contributor to mineral studies at Mont Saint-Hilaire, and author of "The Complete Book of Micromounting" (1993). The 3T polytype was first found at Mont Saint-Hilaire.
A polytype of Quintinite

The 2H polytype was originally described from Jacupiranga alkaline complex, Cajati, São Paulo, Brazil.


Unique IdentifiersHide

Mindat ID:
31536
Long-form identifier:
mindat:1:1:31536:0

Physical Properties of Quintinite-2HHide

Vitreous
Transparency:
Transparent
Colour:
Deep orange-red, orange, pale brown
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{0001}
Fracture:
Irregular/Uneven
Density:
2.14(1) g/cm3 (Measured)    2.15 g/cm3 (Calculated)

Optical Data of Quintinite-2HHide

Type:
Uniaxial (+)
RI values:
nω = 1.533(1) nε = 1.533
Surface Relief:
None to Very Low
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Pleochroism:
Visible
Comments:
ω = yellow, ε = lighter yellow.

Chemistry of Quintinite-2HHide

Mindat Formula:
Mg4Al2(OH)12(CO3) · 3H2O
Element Weights:
Element% weight
O61.362 %
Mg20.715 %
Al11.498 %
H3.866 %
C2.559 %

Calculated from ideal end-member formula.
O
Mg
Al
H
C

Crystallography of Quintinite-2HHide

Crystal System:
Hexagonal
Class (H-M):
622 - Trapezohedral
Space Group:
P6322
Cell Parameters:
a = 10.571 Å, c = 15.171 Å
Ratio:
a:c = 1 : 1.435
Unit Cell V:
1,468.17 ų (Calculated from Unit Cell)
Z:
4
Morphology:
As equant and prismatic crystals displaying the forms {0001} and an {hkil} trapezohedron with or without {1010}.
Twinning:
None observed.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.63 Å(100)
3.785 Å(100)
1.825 Å(20)
Comments:
Jacupiranga alkaline complex, São Paulo, Brazil. Data are from the type description.

Synonyms of Quintinite-2HHide

Common AssociatesHide

Associations Based on Photo Data:
4 photos of Quintinite-2H associated with StrontianiteSrCO3
4 photos of Quintinite-2H associated with PhlogopiteKMg3(AlSi3O10)(OH)2
4 photos of Quintinite-2H associated with MagnetiteFe2+Fe3+2O4
1 photo of Quintinite-2H associated with DolomiteCaMg(CO3)2
1 photo of Quintinite-2H associated with QuintiniteMg4Al2(OH)12(CO3) · 3H2O

Fluorescence of Quintinite-2HHide

Not fluorescent.

Other InformationHide

Notes:
Attacked slightly by 1:1 HCl, more strongly by 1:1 HNO3, and very strongly by 1:1 H2SO4, all with effervescence.
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 Quintinite-2HHide

References for Quintinite-2HHide

Localities for Quintinite-2HHide

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.
Brazil
 
  • São Paulo
    • Cajati
Chao et al. (1997)
Russia
 
  • Irkutsk Oblast
    • Nizhneilimsky District
      • Zheleznogorsk-Ilimsky
Lapis 37 (2)
  • Murmansk Oblast
    • Kovdorsky District
      • Kovdor Massif
Yakovenchuk et al. (2018)
Sweden
 
  • Värmland County
    • Filipstad
      • Långban Ore District
        • Långban Mine
Strand (2016)
 
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