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Schuilingite-(Nd)

A valid IMA mineral species - grandfathered
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About Schuilingite-(Nd)Hide

Formula:
PbCu(Nd,Gd,Sm,Y)(CO3)3(OH) · 1.5H2O
Colour:
Light azure-blue to turquoise-blue
Lustre:
Adamantine
Hardness:
3 - 4
Specific Gravity:
4.74 (Calculated)
Crystal System:
Orthorhombic
Name:
Named schuilingite in honor of Hendrik Jan Schuiling (13 February 1892, Deventer, Netherlands 24 March 1966, Waterloo, Belgium), Chief Geologist at Union Miniere du Haut-Kantanga. The suffix was added in 1987 to follow the Levinson rule, indicating the predominant essential REE.
This page provides mineralogical data about Schuilingite-(Nd).


Unique IdentifiersHide

Mindat ID:
3588
Long-form identifier:
mindat:1:1:3588:6

IMA Classification of Schuilingite-(Nd)Hide

Approved, 'Grandfathered' (first described prior to 1959)
IMA status notes:
Renamed by the IMA
IMA Formula:
Cu2+Pb2+Nd(CO3)3(OH)·1.5H2O
First published:
1947

Classification of Schuilingite-(Nd)Hide

5.DB.20

5 : CARBONATES (NITRATES)
D : Carbonates with additional anions, with H2O
B : With large and medium-sized cations
16b.1.4.1

16b : HYDRATED CARBONATES CONTAINING HYDROXYL OR HALOGEN
1 : AmBn(XO3)pZqxH2O & with (m+n):p = 1:1
11.9.5

11 : Carbonates
9 : Carbonates of Pb, Zr and Th

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

Physical Properties of Schuilingite-(Nd)Hide

Adamantine
Transparency:
Transparent
Colour:
Light azure-blue to turquoise-blue
Streak:
Light blue
Hardness:
3 - 4 on Mohs scale
Cleavage:
Perfect
Perfect on {110}; poor on {100}.
Density:
4.74 g/cm3 (Calculated)

Optical Data of Schuilingite-(Nd)Hide

Type:
Biaxial (-)
RI values:
nα = 1.71 nβ = 1.755 nγ = 1.775
2V:
Measured: 66° , Calculated: 64°
Max. Birefringence:
δ = 0.065
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:
r > v strong
Pleochroism:
Weak
Comments:
X = colorless to pale blue; Y = azure-blue; Z = blue

Chemistry of Schuilingite-(Nd)Hide

Mindat Formula:
PbCu(Nd,Gd,Sm,Y)(CO3)3(OH) · 1.5H2O
Element Weights:
Element% weight
Pb32.423 %
O28.792 %
Nd22.572 %
Cu9.944 %
C5.638 %
H0.631 %

Calculated from ideal end-member formula.
Pb
O
Nd
Cu
C
H

Crystallography of Schuilingite-(Nd)Hide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Cell Parameters:
a = 7.419(2) Å, b = 18.859(3) Å, c = 6.39(1) Å
Ratio:
a:b:c = 0.393 : 1 : 0.339
Unit Cell V:
894.06 ų (Calculated from Unit Cell)
Z:
4
Comment:
Space group: P21cn

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005636Schuilingite-(Nd)Schindler M, Hawthorne F C (1999) The crystal structure of schuilingite-(Nd) The Canadian Mineralogist 37 1463-147019990293
CIF Raw Data - click here to close

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47c : [Carbonates, phosphates, borates, nitrates]

Type Occurrence of Schuilingite-(Nd)Hide

General Appearance of Type Material:
Crystals are acicular, to 1.5 mm, in subparallel aggregates, or in crusts.
Place of Conservation of Type Material:
Royal Museum of Central Africa, Tervuren, Belgium, RMG11.418.
Associated Minerals at Type Locality:

Synonyms of Schuilingite-(Nd)Hide

Other Language Names for Schuilingite-(Nd)Hide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Schuilingite-(Nd) associated with MalachiteCu2(CO3)(OH)2
1 photo of Schuilingite-(Nd) associated with Gysinite-(Nd)PbNd(CO3)2(OH) · H2O
1 photo of Schuilingite-(Nd) associated with HeterogeniteCo3+O(OH)

Related Minerals - Strunz-mindat GroupingHide

5.DB.RigrahamiteNa2Ca2Th2(CO3)4(HCO3)2(OH)4(H2O)7Mon. 2/m : P21/m
5.DB.GrguriciteCaCr2(CO3)2(OH)4 · 4H2OTric. 1 : P1
5.DB.05Para-alumohydrocalciteCaAl2(CO3)2(OH)4 · 6H2O
5.DB.05NasledovitePbMn3Al4(CO3)4(SO4)O5 · 5H2O
5.DB.05'UM1977-02-CO:AlCaH'Ca6Al2(CO3)3O6 · 32H2O
5.DB.05AlumohydrocalciteCaAl2(CO3)2(OH)4 · 4H2OTric. 1 : P1
5.DB.10KochsándoriteCaAl2(CO3)2(OH)4 · H2OOrth. mmm(2/m2/m2/m) : Pnma
5.DB.10DresseriteBaAl2(CO3)2(OH)4 · H2OOrth. mmm(2/m2/m2/m)
5.DB.10DundasitePbAl2(CO3)2(OH)4 · H2OOrth. mmm(2/m2/m2/m)
5.DB.10'Unnamed (Ca-analogue of Petterdite)'CaCr3+2(CO3)2(OH)4 · H2O
5.DB.10PetterditePbCr3+2(CO3)2(OH)4 · H2OOrth. mmm(2/m2/m2/m)
5.DB.10StrontiodresseriteSrAl2(CO3)2(OH)4 · H2OOrth. mmm(2/m2/m2/m)
5.DB.10MontroyaliteSr4Al8(CO3)3(OH,F)26 · 10-11H2OTric.
5.DB.15HydrodresseriteBaAl2(CO3)2(OH)4 · 3H2OTric. 1 : P1
5.DB.25SergeeviteCa2Mg11(CO3)9(HCO3)4(OH)4 · 6H2OTrig.
5.DB.30Szymańskiite[H3O]+8[Hg2]2+8(Ni,Mg)6[CO3]12(OH)12 · 3H2OHex. 6 : P63
5.DB.35Lusernaite-(Y)Y4Al(CO3)2(OH)10F · 6H2O Orth. mmm(2/m2/m2/m) : Pnma
5.DB.40PutnisiteSrCa4Cr3+8(CO3)8SO4(OH)16 · 23H2OOrth. mmm(2/m2/m2/m) : Pnma

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 Schuilingite-(Nd)Hide

References for Schuilingite-(Nd)Hide

Localities for Schuilingite-(Nd)Hide

Showing 3 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
    • Georgiana County
      • Peelwood
Leverett et al. (2007)
DR Congo
 
  • Lualaba
    • Mutshatsha
      • Kamoto
[Mandarino
Lhoest (1992) +1 other reference
 
and/or  
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