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Petersenite-(Ce)

A valid IMA mineral species
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About Petersenite-(Ce)Hide

00737140017271925856135.jpg
Ole V. Petersen
Formula:
Na4(Ce,La,Nd)2(CO3)5
Colour:
Pinkish gray, yellow
Lustre:
Vitreous
Hardness:
3
Crystal System:
Monoclinic
Name:
Named in 1994 by Joel D. Grice, Jerry Van Velthuizen, and Robert A. Gault in honour of Dr. Ole Valdemar Petersen (July 29, 1939, Gentofte, Denmark - March 31, 2020, Solrød, Denmark). Petersen was Curator of the Mineral Collection at The Geological Museum, University of Copenhagen and best known for his work on the mineralogy of alkaline rocks, especially those from Greenland.
A rare-earth-element carbonate.


Unique IdentifiersHide

Mindat ID:
3174
Long-form identifier:
mindat:1:1:3174:1

Similar NamesHide

PattersoniteA valid IMA mineral speciesPbFe33+(PO4)2(OH)5 · H2O
PetersiteA synonym
Petersite-(Ce)A valid IMA mineral speciesCeCu6(PO4)3(OH)6 · 3H2O
Petersite-(La)A valid IMA mineral speciesLaCu6(PO4)3(OH)6 · 3H2O
Petersite-(Y)A valid IMA mineral speciesYCu6(PO4)3(OH)6 · 3H2O
PietersiteA variety of 'Chalcedony' [Quartz]SiO2

IMA Classification of Petersenite-(Ce)Hide

Classification of Petersenite-(Ce)Hide

5.AD.15

5 : CARBONATES (NITRATES)
A : Carbonates without additional anions, without H2O
D : With rare-earth elements (REE)
14.4.5.2

14 : ANHYDROUS NORMAL CARBONATES
4 : Miscellaneous

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

Pronunciation of Petersenite-(Ce)Hide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of Petersenite-(Ce)Hide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Pinkish gray, yellow
Hardness:

Optical Data of Petersenite-(Ce)Hide

Type:
Biaxial (+/-)
RI values:
nα = 1.623 nβ = 1.636 nγ = 1.649
2V:
Measured: 85° to 95°, Calculated: 89.8°
Max. Birefringence:
δ = 0.026
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.
Dispersion:
Weak
Pleochroism:
Non-pleochroic

Chemistry of Petersenite-(Ce)Hide

Mindat Formula:
Na4(Ce,La,Nd)2(CO3)5
Element Weights:
Element% weight
Ce41.687 %
O35.700 %
Na13.680 %
C8.933 %

Calculated from ideal end-member formula.
Ce
O
Na
C

Crystallography of Petersenite-(Ce)Hide

Crystal System:
Monoclinic
Class (H-M):
2 - Sphenoidal
Space Group:
P21
Setting:
P21
Cell Parameters:
a = 20.872 Å, b = 6.367 Å, c = 10.601 Å
β = 120.50°
Ratio:
a:b:c = 3.278 : 1 : 1.665
Unit Cell V:
1,213.85 ų (Calculated from Unit Cell)
Morphology:
Striated prisms; acicular crystals

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005369Petersenite-(Ce)Grice J D, Velthuizen J V, Gault R A (1994) Petersenite-(Ce), a new mineral from Mont Saint-Hilaire, and its structural relationship to other REE carbonates The Canadian Mineralogist 32 405-4141994Mont Saint-Hilaire, Quebec, Canada0293
CIF Raw Data - click here to close

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks

Type Occurrence of Petersenite-(Ce)Hide

Synonyms of Petersenite-(Ce)Hide

Other Language Names for Petersenite-(Ce)Hide

Relationship of Petersenite-(Ce) to other SpeciesHide

Other Members of Burbankite Group:
Burbankite(Na,Ca)3(Sr,Ba,Ce)3(CO3)5Hex. 6mm : P63mc
CalcioburbankiteNa3(Ca,REE,Sr)3(CO3)5Hex. 6mm : P63mc
Khanneshite(Na,Ca)3(Ba,Sr,Ce,Ca)3(CO3)5Hex. 6mm : P63mc
Lishiite(Ca2◻)Sr3(CO3)5Hex. 6mm : P63mc
Rémondite-(Ce)Na3(Ce,Ca,Na)3(CO3)5Mon. 2 : P21
Rémondite-(La)Na3(La,Ca,Na)3(CO3)5Mon. 2 : P21
SanromániteNa2CaPb3[CO3]5Hex. 6mm : P63mc

Common AssociatesHide

Associations Based on Photo Data:
12 photos of Petersenite-(Ce) associated with CalcioburbankiteNa3(Ca,REE,Sr)3(CO3)5
8 photos of Petersenite-(Ce) associated with SideriteFeCO3
8 photos of Petersenite-(Ce) associated with AlbiteNa(AlSi3O8)
6 photos of Petersenite-(Ce) associated with AegirineNaFe3+Si2O6
5 photos of Petersenite-(Ce) associated with Thomasclarkite-(Y)(Na,Ce)(Y,REE)(HCO3)(OH)3 · 4H2O
5 photos of Petersenite-(Ce) associated with GaidonnayiteNa2Zr(Si3O9) · 2H2O
3 photos of Petersenite-(Ce) associated with MicroclineK(AlSi3O8)
3 photos of Petersenite-(Ce) associated with AnalcimeNa(AlSi2O6) · H2O
2 photos of Petersenite-(Ce) associated with FerroceladoniteK(Fe2+Fe3+◻)(Si4O10)(OH)2
2 photos of Petersenite-(Ce) associated with NiveolaniteNaBe(CO3)(OH) · 2H2O

Related Minerals - Strunz-mindat GroupingHide

5.AD.05Sahamalite-(Ce)(Mg,Fe)(Ce,La,Nd)2(CO3)4Mon. 2/m : P21/b
5.AD.15Rémondite-(La)Na3(La,Ca,Na)3(CO3)5Mon. 2 : P21
5.AD.15Rémondite-(Ce)Na3(Ce,Ca,Na)3(CO3)5Mon. 2 : P21
5.AD.20Paratooite-(La)(La,Sr,Ca)4CuCa(Na,Ca)2(CO3)8Orth. mmm(2/m2/m2/m) : Pbam

Fluorescence of Petersenite-(Ce)Hide

No fluorescence

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 Petersenite-(Ce)Hide

References for Petersenite-(Ce)Hide

Localities for Petersenite-(Ce)Hide

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.
Canada (TL)
 
  • Québec
    • Montérégie
      • La Vallée-du-Richelieu RCM
        • Mont Saint-Hilaire
Grice et al. (1994) +1 other reference
Russia
 
  • Murmansk Oblast
    • Koashva Mt
Arzamastsev et al. (2008)
33 IGC excursion No 47
Pekov et al. (1998)
 
and/or  
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