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Decrespignyite-(Y)

A valid IMA mineral species
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About Decrespignyite-(Y)Hide

Formula:
Cu(Y,REE)4(CO3)4(OH)5Cl · 2H2O
Colour:
Bright royal blue to pale blue
Lustre:
Vitreous, Pearly
Hardness:
4
Specific Gravity:
3.64
Crystal System:
Monoclinic
Name:
Honouring Robert James Champion de Crespigny (b. 1950), Chairman of Normandy Mining Ltd. and Chairman of the South Australian Museum, for his contributions to Australian education.
This page provides mineralogical data about Decrespignyite-(Y).


Unique IdentifiersHide

Mindat ID:
9294
Long-form identifier:
mindat:1:1:9294:0

IMA Classification of Decrespignyite-(Y)Hide

Approved
IMA Formula:
Y4Cu2+(CO3)4Cl(OH)5·2H2O
Approval year:
2001

Classification of Decrespignyite-(Y)Hide

5.CC.35

5 : CARBONATES (NITRATES)
C : Carbonates without additional anions, with H2O
C : With rare earth elements (REE)
16a.1.11.1

16a : ANHYDROUS CARBONATES CONTAINING HYDROXYL OR HALOGEN
1 : (AB)(XO3)Zq

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

Physical Properties of Decrespignyite-(Y)Hide

Vitreous, Pearly
Colour:
Bright royal blue to pale blue
Streak:
Pale blue
Hardness:
Comment:
Estimated
Fracture:
None observed
Density:
3.64 g/cm3 (Measured)    3.645 g/cm3 (Calculated)

Optical Data of Decrespignyite-(Y)Hide

Type:
Biaxial (-)
RI values:
nα = 1.604(4) nγ = 1.638(3)
Max. Birefringence:
δ = 0.034
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.

No measured or calculated 2V is on file for this mineral, so the value used here (89°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Pleochroism:
Visible
Comments:
Medium strong; X very pale bluish, Y and Z bluish (with greenish tint)

Chemistry of Decrespignyite-(Y)Hide

Mindat Formula:
Cu(Y,REE)4(CO3)4(OH)5Cl · 2H2O
Element Weights:
Element% weight
Y43.596 %
O37.266 %
Cu7.790 %
C5.890 %
Cl4.346 %
H1.112 %

Calculated from ideal end-member formula.
Y
O
Cu
C
Cl
H

Crystallography of Decrespignyite-(Y)Hide

Crystal System:
Monoclinic
Cell Parameters:
a = 8.899(6) Å, b = 22.77(2) Å, c = 8.589(6) Å
β = 120.06(5)°
Ratio:
a:b:c = 0.391 : 1 : 0.377
Unit Cell V:
1506.3 ų
Z:
4
Morphology:
As crusts, coatings and fillings in thin fissures on the slatey country rock.
Comment:
powder Diffraction data indicate the space group is P2, Pm or P2/m. New data by Rius et al. (2020) suggest space group P-3m1 and a= 8.5462(2), c= 22.731(2) Å, but these authors cannot exclude monoclinic symmetry and their model contains several partially occupied sites (disorder is indicated by streaks).

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
22.79 Å(30)
7.463 Å(30)
7.086 Å(50)
6.241 Å(100)
4.216 Å(30)
3.530 Å(40)
3.336 Å(30)
2.143 Å(30)

Type Occurrence of Decrespignyite-(Y)Hide

General Appearance of Type Material:
Blue crusts, coatings and fillings in thin fissures. Crusts and spherulitic aggregates are composed of individual tiny pseudohexagonal, often curved platelets.

Synonyms of Decrespignyite-(Y)Hide

Other Language Names for Decrespignyite-(Y)Hide

Simplified Chinese:碳氯钇铜矾
Traditional Chinese:碳氯釔銅礬

Common AssociatesHide

Associations Based on Photo Data:
21 photos of Decrespignyite-(Y) associated with Kamphaugite-(Y)Ca(Y,REE)(CO3)2(OH) · H2O
9 photos of Decrespignyite-(Y) associated with MalachiteCu2(CO3)(OH)2
7 photos of Decrespignyite-(Y) associated with Tengerite-(Y)Y2(CO3)3 · 2-3H2O
2 photos of Decrespignyite-(Y) associated with Donnayite-(Y)NaCaSr3Y(CO3)6 · 3H2O
2 photos of Decrespignyite-(Y) associated with Alicewilsonite-(YLa)Na2Sr2YLa(CO3)6 · 3H2O
2 photos of Decrespignyite-(Y) associated with CalciteCaCO3

Related Minerals - Strunz-mindat GroupingHide

5.CC.Bainbridgeite-(NdCe)Na2Ba2NdCe(CO3)6 · 3H2OTric. 1 : P1
5.CC.Yuchuanite-(Y)Y2(CO3)3 · H2OTric. 1 : P1
5.CC.Alicewilsonite-(YCe)Na2Sr2YCe(CO3)6 · 3H2OTric. 1 : P1
5.CC.05Donnayite-(Y)NaCaSr3Y(CO3)6 · 3H2OTric. 1 : P1
5.CC.05Alicewilsonite-(YLa)Na2Sr2YLa(CO3)6 · 3H2OTric. 1 : P1
5.CC.05Mckelveyite-(Nd)NaCaBa3Nd(CO3)6 · 3H2OMon. m : Bb
5.CC.05Mckelveyite-(Y)NaCaBa3Y(CO3)6 · 3H2OTric. 1 : P1
5.CC.05EwalditeBa(Na,Ca,Y,Ce,K)(CO3)2 · 2.6H2OHex. 6mm : P63mc
5.CC.05'UM1992-05-CO:CaCeLaNaSr'(Sr,Na,Y,REE,Ca,Ba)2(CO3)2 · H2OTrig. 3m : R3m
5.CC.05WeloganiteNa2Sr3Zr(CO3)6 · 3H2OTric. 1 : P1
5.CC.05Mckelveyite GroupA3B3(CO3)6 · 3H2O
5.CC.05Bainbridgeite-(YCe)Na2Ba2YCe(CO3)6 · 3H2OTric. 1 : P1
5.CC.05'Unnamed (MSH UK-37A)'Sr3NaCaY(CO3)6 · 3H2OHex. 6mm : P63mc
5.CC.10Tengerite-(Y)Y2(CO3)3 · 2-3H2OOrth. mmm(2/m2/m2/m) : Pnnm
5.CC.15Lokkaite-(Y)Ca(Y,Gd,Nd,Dy)4(CO3)7 · 9H2OOrth.
5.CC.15Kimuraite-(Y)Ca(Y,Nd)2(CO3)4 · 6H2OOrth.
5.CC.15Hizenite-(Y)Ca2Y6(CO3)11 · 14H2O Orth.
5.CC.20Shomiokite-(Y)Na3Y[CO3]3 · 3H2OOrth. mm2
5.CC.25Lanthanite-(Ce)Ce2(CO3)3 · 8H2OOrth. mmm(2/m2/m2/m)
5.CC.25Lanthanite-(La)La2(CO3)3 · 8H2OOrth. mmm(2/m2/m2/m)
5.CC.25Lanthanite-(Nd)Nd2(CO3)3 · 8H2OOrth. mmm(2/m2/m2/m)
5.CC.25Calkinsite-(Ce)(Ce,La)2(CO3)3 · 4H2OOrth.
5.CC.30Adamsite-(Y)NaY[CO3]2 · 6H2OTric. 1 : P1
5.CC.40Galgenbergite-(Ce)Ca(Ce,La,Nd)2(CO3)4 · H2OTric. 1 : P1
5.CC.45Lecoqite-(Y)Na3Y(CO3)3 · 6H2OHex. 6 : P63

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 Decrespignyite-(Y)Hide

References for Decrespignyite-(Y)Hide

Localities for Decrespignyite-(Y)Hide

Showing 1 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 (TL)
 
  • South Australia
    • District Council of Peterborough
      • Paratoo
Kolitsch et al. (2026) +2 other references
 
and/or  
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